Post-Caldera Volcanism in Yellowstone National Park

Home , Caldera, Huckleberry Ridge Tuff, Lava Creek Tuff, Overhanging Cliff, Roaring Mountain, Sheepeater Cliff

POST-CALDERA VOLCANISM IN YELLOWSTONE NATIONAL PARK:

PETROGENESIS OF THE INTRACALDERA UPPER BASIN

MEMBER OF THE PLATEAU RHYOLITE AND

EXTRA-CALDERA MINGLED MAGMA

COMPLEXES

CHAD JAMES PRITCHARD

A dissertation submitted in partial fulfillment of The requirements for the degree of

Doctor of Philosophy

WASHINGTON STATE UNIVERSITY School of Earth and Environmental Sciences

MAY 2011

To the Faculty of Washington State University:

The members of the Committee appointed to examine the dissertation of CHAD JAMES PRITCHARD find it satisfactory and recommend that it be accepted.

Peter B. Larson, Ph.D., Chair

Terry L. Spell, Ph.D.

John A. Wolff, Ph.D.

ACKNOWLEDGMENTS

I could have only conducted this research with the support and understanding of my wife,

Meghan Lunney, of whom I am super-duper grateful. Peter Larson, chair of this committee, was extremely helpful and kind, which is greatly appreciated. I would also like to thank the other members of my committee for their time and energy. World class assistance in the field was given by Allen

Anderson, William Starkel, and Kevin Tarbert. Sample analyses were conducted at Washington State

University GeoAnalytical Laboratories with appreciated help from Dr. Rick Conrey, Charles Knaack, Dr.

Garret Hart, and Dr. Jeffery Vervoort. Sampling permits were issued by Yellowstone National Park,

Research Permit Office, with help from Christie L. Hendrix. Acknowledgments specific to each research project are present for Chapters 2 and 3. I would also like to thank the kindly folks and friends in the

School of Earth and Environmental Sciences. This study was funded by National Science Foundation grant #EAR-0609475, awarded to Dr. Peter B. Larson; the Washington State University Graduate School; and by the School of Earth and Environmental Sciences, Washington State University.

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POST-CALDERA VOLCANISM IN YELLOWSTONE NATIONAL PARK:

PETROGENESIS OF THE INTRACALDERA UPPER BASIN

MEMBER OF THE PLATEAU RHYOLITE AND

EXTRA-CALDERA MINGLED MAGMA

COMPLEXES

ABSTRACT

by Chad James Pritchard, Ph.D. Washington State University May 2011

Chair: Peter B. Larson

The Plateau Rhyolite erupted following the last large Yellowstone caldera collapse and may have erupted from a rejuvenating magmatic system. Our preferred model for rhyolite genesis is by assimilation of continental crust by mafic magmas, followed by fractional crystallization. This model focuses on the extra-caldera mingled magma complexes and the eastern Upper Basin Member. Radiogenetic isotope trends of the mingled magma complexes show that the rhyolite and basalt portions are isotopically distinct and that cryptic mixing between rhyolite and basalt may have occurred in a number of other extra-caldera rhyolites. Rhyolites of the eastern Upper Basin Member contain petrologic textures and increased radiogenic 87Sr/86Sr in plagioclase phenocrysts (0.7134 to 0.7185) when compared to the groundmass and whole rock radiogenic values (0.7099 to 0.7161). δ18O depletions on the order of 5‰ found in the Tuff of Sulphur Creek and Canyon flow indicate at least a two-stage petrogenesis involving assimilation and fractional crystallization. The presence of a low-δ18O rhyolite outside the caldera indicates that country rock was hydrothermally altered at depth and then assimilated to form the

Dunraven Road flow.

TABLE OF CONTENTS

Page ACKNOWLEDGMENTS ...... iii

ABSTRACT ...... iv

LIST OF TABLES ...... viii

LIST OF FIGURES ...... ix

CHAPTER 1 Introduction to the Geology of the Yellowstone Plateau Area

1. Introduction ...... 1

2. Geologic Background ...... 4

3. History of Volcanism – Yellowstone Caldera ...... 6

4. Geothermal History...... 10

5. Whole Rock Geochemistry ...... 11

6. Isotopes ...... 15

7. EC-RAxFC Models ...... 16

8. Summary of Conclusions From This Dissertation ...... 21

9. References ...... 22

CHAPTER 2 Mixed magma complexes and extra-caldera volcanism in the Norris-Mammoth Corridor

1. Abstract ...... 28

2. Introduction ...... 29

3. Geologic Background ...... 31

4. Material and Methods ...... 32

5. Results ...... 36

6. Discussion ...... 48

7. Acknowledgments ...... 51

8. References ...... 52

CHAPTER 3 Evolution of the Upper Basin Member of the Plateau Rhyolites

1. Abstract ...... 57

2. Introduction ...... 57

3. Sampling and Methods ...... 63

4. Results ...... 69

5. Discussion ...... 86

6. Conclusions ...... 96

7. Acknowledgments ...... 97

8. References ...... 98

APPENDICES

A. WHOLE ROCK MAJOR AND TRACE ELEMENT DATA ...... 104

B. RESULTS FROM EC-RAxFC MODELS ...... 130

C. RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF FELDSPAR FROM THE MINGLED

MAGMAS...... 151

D. RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF XENOCRYSTS FROM THE

MINGLED MAGMAS ...... 204

E. RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF PYROXENE FROM THE MINGLED

MAGMAS...... 209

F. RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF OLIVINE FROM THE MINGLED

MAGMAS...... 223

G. RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF GROUNDMASS FROM THE

MINGLED MAGMAS ...... 234

H. RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF GROUNDMASS GLASS FROM

THE EUBM ...... 263

I. RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF GLASS FEATURES FROM THE

EUBM ...... 281

J. RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF PLAGIOCLASE FROM THE

EUBM ...... 291

K. RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF SANADINE FROM THE

EUBM ...... 306

L. RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF PYROXENE FROM THE

EUBM ...... 324

M. RESOURCES FOR CHAPTER 3 – MAJOR ELEMENT DATA FROM THE EUBM ...... 329

N. RESOURCES FOR CHAPTER 3 – OXYGEN ISOTOPE RATIOS FROM THE EUBM ...... 336

O. RESOURCES FOR CHAPTER 3 – LASER ABLATION OF PLACIOGLCASE, 87SR/86SR FROM THE

EUBM ...... 338

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LIST OF TABLES

1. Summary of major eruptive history from the Yellowstone Plateau ...... 7

2. Table of caldera forming eruptions...... 8

3. EC-RAxFC thermal parameters for models...... 19

4. EC-RAxFC compositional parameters ...... 20

5. Post Lava Creek Tuff, extra-caldera volcanic units...... 30

6. Whole rock data from mingled magma complexes ...... 33

7. Average feldspar geochemistry of mingled magma complexes ...... 38

8. Average whole rock analyses of EUBM...... 65

9. Major and trace elements and radiogenic isotope ratios for UBM ...... 66

10. Average feldspar chemistry from the EUBM ...... 68

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LIST OF FIGURES

1. Estimated extent of ash from the three major Yellowstone eruptions...... 2

2. Map of Yellowstone Plateau with post-caldera rhyolites ...... 4

3. Section of Lava Creek Tuff transition...... 9

4. Total Alkalis versus silica plot...... 12

5. Sc versus Ba of Yellowstone volcanic rocks ...... 13

6. Sr versus Ba from the Yellowstone Plateau Area...... 13

7. Sr versus Ba for samples from the EUBM ...... 14

8. Rare earth element diagram for the EUBM...... 14

9. 87Sr/86Sr ratios versus age in millions of years...... 15

10. 206Pb/204Pb ratios versus δ 18O ratios...... 16

11. Radiogenic isotope ratios, Nd vs. Sr. Results from five EC-RAxFC models...... 18

12. 87Sr/86Sr versus temperature (oC) for Model A...... 20

13. Map of Yellowstone National Park and mingled magmas...... 30

14. Photos from the Grizzly Lake complex...... 38

15. Total alkali vs. silica diagram...... 41

16. Al2O3 and viscosity versus SiO2...... 42

17. Ternary diagrams from mingled magma complexes ...... 44

143 144 87 86 18. Nd/ Nd versus Sr/ Sr(initial) graphs...... 47

19. Conceptual model for the development of mingled magma complexes...... 50

20. Map of Yellowstone Volcanic Area...... 59

21. Generalized cross section of the eastern Upper Basin Member rhyolites...... 71

22. Map of the Dunraven Road flow...... 73

23 Rare Earth Element plot for whole rock samples from the EUBM ...... 75

24. Anti-rapakivi diagram...... 77

25. Photomicrographs from the EUBM ...... 78

87 86 147 144 26. Sr/ Sr (480ka) and Nd/ Nd plot of rhyolitic groups from Yellowstone ...... 82

27. Measured 208Pb/204Pb and 207Pb/204Pb versus 206Pb/204Pb plots...... 83

28. Results from laser 87Sr/86Sr for plagioclase ...... 84

29. Generalized cartoon of development of UBM rhyolites ...... 95

CHAPTER 1

INTRODUCTION TO THE GEOLOGY OF THE YELLOWSTONE PLATEAU AREA

Introduction

The Yellowstone Plateau is located in the northwest corner of Wyoming and portions of Montana and Idaho. Volcanic eruptions from the Yellowstone Plateau are volumetrically dominated by three large caldera-forming eruptions initiated 2.05 Ma (Lanphere et al., 2002). These catastrophic eruptions likely affected the global climate as ash deposits have been found across the United States (Lowenstern et al.,

2006). Numerous groups of smaller eruptions prior to and following the larger eruptions help us understand how such large magma systems develop. Eruptions could still occur in the active caldera system at Yellowstone (Christiansen et al., 2007). Using GIS, seismic tomography, and volatile gas geochemistry provide data to develop models for current magmatic activity (Lowenstern et al., 2006).

Using petrology and geochemistry this paper attempts to develop a model to help understand how the magmatic system may have acted over the last 640,000 years, or since the last caldera collapse, which may be used to understand how large-scale magmatic systems develop over time. Therefore, it is also important to understand the chemical composition and character of erupted material from the Yellowstone magmatic system. Chapter 2 is an analysis of the mingled magma complexes north of the caldera.

Chapter 3 is a summary of both physical and geochemical research of the Upper Basin Member and models for magma chamber cycles found in the Yellowstone caldera.

The most recent large, caldera forming, eruption led to the deposition of the Lava Creek Tuff, approximately 640 ± 2 ka (Lanphere et al., 2002). A series of rhyolites within (intracaldera) and outside the caldera (extra-caldera) have been emplaced in the following 640,000 years (Table 1). These units are collectively referred to as the “Plateau Rhyolite”. Extra-caldera volcanism also includes numerous basalt flows and mingled magma complexes.

Figure 1. Estimated extent of ash from the three major Yellowstone eruptions. Outline of the United States of America with location of the Yellowstone Plateau. From Christiansen et al. (2007).

Past research has focused on the mapping and geochemistry of caldera-forming eruptions and general studies of smaller eruptions from within the caldera (Iddings, 1899; Boyd, 1961; Christensen and

Blank, 1975; Doe et al., 1982; Hildreth et al., 1984; Hildreth et al., 1991; Christiansen, 2001). More detailed work on the Plateau Rhyolite has been conducted on the younger Central Plateau Member

(Vasquez and Reid, 2002; Vasquez et al., 2009; Girard and Stix, 2010) and on the oldest of the intracaldera rhyolites, the Upper Basin Member (Bindeman and Valley 2001; Bindeman et al., 2008;

Girard and Stix, 2009). The Upper Basin Member has been divided into the eastern Upper Basin rhyolites (EUBM), including the Tuff of Uncle Tom’s Trail, Tuff of Sulphur Creek, Canyon Flow, and

Dunraven Road Flow, and the western Upper Basin rhyolites (WUBM), including the Biscuit Basin

Flows and Scaup Lake Flow (Gansecki et al., 1996). Christiansen et al. (2007) summarized the ages for rhyolites and basalts in the Yellowstone Plateau. Locations of the calderas and Plateau Rhyolite are presented in Figure 2.

Basalt in the Yellowstone Plateau Area is exclusively found as extra-caldera flows, though any older flows within the caldera would have most likely been covered by a thick coating of Plateau

Rhyolites. The most comprehensive studies of extra-caldera units were conducted by Bennet (2002) for the basaltic portions and by Nastanski (2002) for the rhyolites. A summary of major eruption history is presented in Table 1. Studying the flows that followed the last caldera formation is very important as they are the manifestation of a still active magmatic system and can be used to understand how the system changes with time.

The first portion of this study is concerned with the mingled magmas present north of the caldera, along the Norris-Mammoth corridor. These units provide a unique opportunity to study the petrogenesis and mingling of basalts and rhyolites from the Yellowstone Plateau Area. Mingled magmas of the

Gardner River and Grizzly complex have been well known to the scientific community since the 1800’s

(Iddings, 1899; Fenner, 1938, 1944; Wilcox, 1944). Classically the complexes are considered mixed; however, the presence of mafic enclaves suggests that the term, “mingled” may better describe the four recognized mingled magma complexes, which are further discussed in Chapter 2 of this dissertation.

The second portion of this study focuses on the eastern Upper Basin Member of the Plateau rhyolites (EUBM), located just within the northeastern ring fracture north of the Sour Creek resurgent

Dome (Figure 2). These flows are low-δ18O high-silica rhyolites (Hildreth, 1984; Bindeman and Valley,

2001; Bindeman et al., 2008). Generally, these flows contain 10 to 35 percent phenocrysts (Girard and

Stix, 2009; Larson et al., 2009). However, the youngest of the EUBM, the Dunraven Road Flow, contains fewer phenocrysts, less than 8 percent (Girard and Stix, 2009). This study addresses petrology, isotope geochemistry, and field observations to determine the petrogenesis of the EUBM in Chapter 3.

Figure 2. Map of Yellowstone Plateau with post-caldera rhyolites. Dotted outlines denote the approximate outline of the three calderas in Yellowstone. The Mallard Lake Dome and Sour Creek Dome are resurgent domes. The Upper Basin Member

(orange), Central Plateau Member (pink), and extra-caldera rhyolites (brown) make up the Plateau Rhyolite. Map from Pritchard and Larson (in review).

Geologic Background

It is useful to evaluate the characteristics of materials that are potentially being assimilated or contaminating magmas, when considering how high silica rhyolites formed. At Yellowstone the bedrock lithologies may consist of the Archean southern Beartooth Mountain Block, Paleozoic to Mesozoic shallow marine sedimentary rocks, and Eocene Absaroka mafic to intermediate volcanic rocks and lahar deposits. Mapping of these units has been compiled by Christiansen (2001) and was used for the following section.

The southern block of the Beartooth Mountains, located in northern portion of the park, is comprised of granodiorites, gneissic granites to granodiorites, andesitic amphibolites, and granite biotite schists. They are estimated to have formed approximately 2.8 Ga based on U-Th ages of zircons

(Wooden and Mueller, 1988; Christiansen, 2001). During our field work we observed gneissic granites, garnet-biotite schists, norites, and migmatites in the northern portion of the park.

The Mississippian Madison limestone outcrops extensively in the northeastern corner of the park and to the south of the caldera. Other sedimentary units have also been mapped, for example the

Mississippian Lodgepole limestone, Devonian Three Forks and Jefferson clastic formations, Ordovician

Bighorn Dolomite and older Cambrian sedimentary units (Love and Keefer, 1975; Prostka et.al., 1975;

Christiansen, 2001). The presence of deeper sedimentary bedrock outside of the caldera ring fracture zone is suggested by hydrocarbons in the Washburn hot springs (Fournier, 1989) and by CO2 emissions

(Werner and Brantley, 2003).

Eocene Absaroka volcanics are present around the northeastern corner of the Yellowstone caldera. These Eocene magmas intruded the deep continental crust and then mixed within shallow reservoirs (Feeley et al., 2002). Exposed stocks of the Eocene Mt. Washburn volcano, just north of the

EUBM outcrops, indicate that the southern portion of the edifice foundered into the caldera during collapse (Feeley et al., 2002). Lithic fragments of the Mt. Washburn volcanics are present in the Tuff of

Uncle Tom’s Trail (Christiansen, 2001). Xenocrysts in some of the Upper Basin Member rhyolites may have originated from Eocene volcanic rocks (Gansecki et al., 1996)

Archean development of the Yellowstone region may have included multiple periods of orogenic compressional tectonics, with early subduction to the west, later changing to northly dipping subduction between 3.8 to 2.6 Ga (Clowes et al., 2002). Subsequent orogenies have transpired, including the east- west compression of the Laramide orogeny, uplifting blocks of Precambrian basement (Beartooth

Mountains), and older sedimentary rocks.

Tectonically, the caldera has three major characteristics. First, Yellowstone is located at the north eastern end of the Snake River Plain, or at the current eastern terminus of the Snake River – Yellowstone hot spot track, or thermal anomaly. The Snake River Plain is a topographic depression that acts as a tectonic axis from southern Oregon to the Yellowstone caldera. Second, multiple north-south trending normal faults from the Basin and Range province are exposed north and south of the caldera. These active extensional faults anomalously change direction on either side of the caldera, forming a tectonic parabola (Smith & Braile, 1994). Finally, Yellowstone is located over older thrust faulting and folding from the late Cretaceous and early Tertiary orogenies.

Magmatism in Yellowstone may be driven by extensive basaltic intrusions caused by the Snake

River Plain – Yellowstone thermal anomaly, or hotspot (Nash et al., 2006). However, there are also different views that suggest other mechanisms, such as upper mantle convection (Christiansen et al.,

2002), or decompression melting associated with Basin and Range structures (Leeman et al., 2009).

Geophysical imaging, currently being compiled for the USArray Investigation, suggests the crust and mantle are indeed warm below Yellowstone, but that the heated area is planar and has a slope dipping to the north.

History of Volcanism – Yellowstone Caldera

The late Cenozoic volcanism at Yellowstone included three major caldera forming eruptions that deposited 1) the Huckleberry Ridge Tuff (2.053 Ma), 2) the Mesa Falls Tuff (1.292 Ma), and 3) the most recent Lava Creek Tuff (639 ka), as shown in Table 2. This yields a recurrence interval of approximately

600 to700 ka for caldera forming eruptions (Christiansen et al., 2007). Initial mapping of the

Yellowstone caldera identified the volcanic/tectonic origin for the area and grouped the Huckleberry

Ridge Tuff and Lava Creek Tuff into one unit, called the Yellowstone Formation (Boyd, 1961).

Approximate locations of the three major caldera collapse sequences are presented in Figure 2. Deposits from the three caldera forming eruptions are termed, “The Yellowstone Group.” (Christiansen, 2001)

Lower magnitude volcanism (<200 km3 of magma per eruption) is also prevalent as pre and post caldera forming eruptions. Rhyolitic domes, flows, and pyroclastic deposits have been eroded to form multiple plateaus within the caldera (intracaldera) and are also present outside of the caldera. Basaltic lavas erupted before and after each of the caldera forming eruptions and are generally restricted to extra- caldera settings, although it is possible that basalt eruptions followed large scale eruption and were then covered by intracaldera rhyolites. Along the Norris- Mammoth Corridor, north of the caldera, there are also multiple examples of mingled magmas, where basalt and rhyolite erupted at the same time (units in the Obsidian Creek Member of the Plateau Rhyolite). A stratigraphic table of the volcanic history is presented below (Table 1).

Table 1. Summary of major eruptive history from the Yellowstone Plateau and Island Park area, in stratigraphic order. Table

modified from Christiansen (2001).

Caldera-forming Contemporaneous Volcanic Precaldera ash flow tuff Postcaldera Age plateau marginal Cycle rhyolites “Yellowstone rhyolites basalts Group” Basalt of Snake River Plateau Rhyolites: Osprey basalt Members: Madison River basalt Basalt of Geode Creek -Central Plateau -Obsidian Creek** Swan Lake Flat basalt -Roaring Mountain** Gerrit basalt Third -Upper Basin Falls River basalt Basalt of Mariposa Lake Pleistocene Lava Creek Tuff (0.01 to 2 Mount Jackson Ma) rhyolite Undine Falls basalt Basalt of Warm River Lewis Canyon Basalt of Shotgun Valley rhyolite Island Park rhyolite Basalt of the Narrows

Mesa Falls Tuff Second Big Bend Ridge

rhyolite* Big Bend Ridge

rhyolite*

Pliocene Huckleberry Ridge (2 to 5.9 First Tuff Ma) Rhyolite of Snake Jackson Butte Basalt River Butte * Note that a portion of Big Bend Ridge rhyolite is considered a post-caldera and another portion considered pre-caldera rhyolites. **Ages of Roaring Mountain and Obsidian Creek Members of the Plateau Rhyolites also have younger portions that predate the youngest flows of the Central Plateau. The oldest flow is the Overhanging Cliff flow, part of the Jackson Butte basalt (2.16 Ma) and the youngest flow is Pitchstone Plateau Flow, part of the Central Plateau Member of the Plateau Rhyolite (70 ka) (Christiansen, 2001).

The initial volcanism of the Yellowstone caldera, approx 2.16 Ma, was basaltic and followed by successive rhyolites and basalts until the eruption of the Huckleberry Ridge Tuff. This eruption may have created three separate calderas, the first (member A) was located near where the Mallard Lake Dome currently stands, the second of the eruptions (member B) was from Island Park (Idaho), and the last eruption may have produced a caldera in the southwest corner of Yellowstone National Park, near where the Pitchstone Plateau (Central Plateau Member) is currently located (Christiansen, 2001). Member C of the Huckleberry Ridge Tuff is described as only comprising 290 km3, which is relatively small compared to members A and B (Table 2). A number of smaller rhyolite eruptions deposited the Big Bend rhyolites, during the following 760,000 years, until the second caldera forming eruption deposited the Mesa Falls tuff. Although the Mesa Falls tuff was deposited by a caldera forming eruption, this eruption is thought to be much smaller and west of the current Yellowstone caldera (Christiansen, 2001). A series of basalts and rhyolites followed the Mesa Falls Tuff and predated the eruption of the Lava Creek Tuff. Rhyolites and basalts following the deposition of the Mesa Falls Tuff were generally erupted from the Island Park area and south of the current caldera, although Undine Falls basalt is found north of the caldera.

Table 2. Table of caldera forming eruptions.

Unit Age (Ma)* Approximate Volume (km3)** Member B: 490 Lava Creek Tuff 0.639 ± 0.002 Member A: 510 Mesa Falls Tuff 1.285 ± 0.004 280 Member C: 290 Huckleberry Ridge 2.059±0.004 Member B: 1,340 Tuff Member A: 820 40 39 * Ages estimated using Ar- Ar (Lanphere et al., 2002) **approximate volumes (Christiansen, 2001).

The Lava Creek Tuff is comprised of at least two separate eruptions, members A and B.

Christiansen and Blank (1972) describe a reversal in welding in the central portion of the tuff, which indicates a cooling break (Figure 3). Each of the eruptions that deposited the Lava Creek Tuff effused from vents located very near the current resurgent domes of the caldera (Christiansen, 2001). The eruptions were most likely closely spaced in time as there have been no observed signs of erosion or soil development at the contact between the members. Following the deposition of the Lava Creek Tuff the

Plateau Rhyolite filled the caldera to form the current Yellowstone Plateau overflowing the southwest boundary of the current caldera. Extra-caldera rhyolite and basalt flows erupted north of the caldera along the Mammoth Corridor, to the west in Island Park, with one eruption south of the caldera.

Figure 3. Section of Lava Creek Tuff transition between member A and member B, from along the Virginia Cascade pullout in central Yellowstone National Park. Figure from Christiansen (2001).

Geothermal History

There are two important reasons to understand the hydrothermal system at the Yellowstone caldera. First, the active hydrothermal system is thought to be driven by heat from a crystallizing magma chamber at least 8 km below the caldera as imaged using seismic tomography (Husen et al., 2004).

Therefore, the caldera still shows signs of being active. Second, post-caldera rhyolites have a low-δ18O signature that is indicative of meteoric hydrothermal alteration of source rocks (Friedman et al., 1974).

Yellowstone hosts one of the largest currently active hydrothermal systems found in the world

(Christiansen et al., 2007). 40Ar/39Ar ages of alunite in the Canyon area of Yellowstone suggests that hydrothermal systems have been in place prior to 150 ka (Larson et al., 2009); though the hydrothermal systems have most likely been active prior to that time. Regardless of the age, a hydrothermal system requires an ample water supply, sufficient permeability in the surrounding rocks to allow infiltration of water and cycling of heated water, and a heat source.

Yellowstone National Park is located along the Continental Divide, in the Rocky Mountains.

According to dendrochronology Yellowstone receives an average annual precipitation of approximately

400 mm between 1200 and 2000 AD (Gray et al., 2006). The elevation also allows for the storage of water for most of the year in the form of ice, and the presence of till deposits and glacial erosion features indicate that the area has been heavily glaciated during the Pleistocene. Hydrothermal systems have been described as being dominated by meteoric waters, due to the low-δ18O values found at Yellowstone

(White, 1969), and driven by the large magmatic anomaly below Yellowstone (Fournier, 1989).

Since the country rock in the area is thought to be crystalline rock and rhyolites tend to have high porosity, but low permeability, it would make sense that the water supply to the hydrothermal systems moves through fractures (Fetter, 1994). However, pervasive hydrothermal alteration through massive rhyolites obviously occurs, as can be seen in the Canyon Area of Yellowstone. Christiansen (2001) points out the strong correlation of extensional structures (i.e., ring fracture and Norris-Mammoth

Corridor) with hydrothermal deposits. Hydrothermal deposits north of the caldera transition to cooler travertine deposits as the hydrothermal system moved north and away from the magmatic heat source.

One of the main questions for this paper is how deep can the meteoric water infiltrate to establish a low-

δ18O hydrothermally altered source rock for rhyolites.

Whole Rock Geochemistry

Whole rock geochemistry is discussed in depth by Christiansen (2001). Appendix A contains whole rock geochemical data collected during this study. Microprobe data from glass and minerals are presented in following chapters and the respective appendices. Results from this study were compared to published geochemistry from the Yellowstone Plateau. Data presented below has been collected from various studies and in some cases uses similar methods, but analysis can date back to the 1950s. The variability between units was commonly similar to the variability of multiple samples within the same unit. Figure 4 is a total-alkali versus silica plot that illustrates the differences between basalt and rhyolite.

The mingled magmas (Chapter 2) are also plotted as intermediate rocks, and Archean basement is also plotted for comparison.

Yellowstone basalts are generally tholeiitic and rhyolites are generally high silica (>75 weight percent

SiO2). Basalts are not observed within the caldera. Intermediate volcanic rocks are generally not found in Yellowstone, aside from the mingled magma complexes as described in Chapter 2. Trace element concentrations are highly variable within each unit and between units. The EUBM and HRT are geochemically distinct from other Yellowstone Area volcanics in the trace elements, Sr, Sc, and Ba

(Figures 5, 6, and 7). Elevated concentrations of TiO2 (weight percent) and Sc (ppm) were previously documented by Hildreth et al. (1984). Rare earth elements (REE) are generally more enriched in the

EUBM samples than other intracaldera rhyolites; however, there is a great deal of variation within each flow, unit, and group of the Plateau Rhyolite. REE patterns for the EUBM are illustrated in Figure 8.

Trace element modeling suggests that these rhyolites were produced by an approximately 30% partial melt of crustal material. However, in subsequent chapters we will discuss the plausibility of partial melting in relation to spatial and temperature constraints and further suggest that assimilation and fractional crystallization may be involved in the formation of these rhyolites.

As will be addressed further in Chapter 3, older EUBM rhyolite have increased Ba and Sr compared to younger EUBM rhyolites and the Dunraven Road flow (Figure 7). The Dunraven Road flow is more homogeneous than most flows, but also contains about the average Ba and Sr of the Yellowstone

Plateau, or less than other EUBM rhyolites (Figures 6 and 7). Discernable differences between the rhyolites are observed in isotopic ratios.

Figure 4. Total Alkalis versus Silica plot. PC - intrusive Archean basement rocks and plot as diorite to granite. Data compiled from Hildreth et al. (1984 and 1991), Christiansen (2001), Bindeman and Valley (2001), and this study.

Figure 5. Sc versus Ba of Yellowstone volcanic rocks, Eocene Mt. Washburn basaltic andesites (Feeley et al., 2002), and

Archean Gneiss of Lamar Canyon and the Beartooth Mts. Data compiled from Hildreth et al. (1984 and 1991), Christiansen

(2001), Bindeman and Valley (2001), and this study.

Figure 6. Sr versus Ba from the Yellowstone Plateau Area. LCT – Lava Creek Tuff, MFT – Mesa Falls Tuff, HRT –

Huckleberry Ridge Tuff. Data compiled from Hildreth et al. (1984 and 1991), Christiansen (2001), Bindeman and Valley (2001), and this study.

Figure 7. Sr versus Ba for samples from the EUBM. Units are subdivided based upon the lithology of the sample. Further discussion of lithology is presented in Chapter 2.

Figure 8. Rare Earth Element diagram for the EUBM. Samples were normalized to BSE – Bulk Silicate Earth (McDonough &

Sun, 1995).

Isotopes

Hildreth et al. (1991) describe “normal” Yellowstone rhyolites and compare the isotopic ratios of different rhyolites with time. Rhyolites following the major caldera collapses of Yellowstone generally have lower δ18O values, and elevated radiogenic 87Sr/86Sr, 206Pb/204Pb, and 207Pb/204Pb ratios relative to other Yellowstone rhyolites. Figure 9 illustrates changes in 87Sr/86Sr ratios with time. Huckleberry Ridge

Tuff, member C (HRT-C) contains more radiogenic 87Sr/86Sr, 206Pb/204Pb, 207Pb/204Pb, and lower

144Nd/143Nd ratios when compared to other Yellowstone volcanics, including the EUBM. However, HRT-

C has a normal δ18O signature. This study has also made the observation that within the UBM rhyolites younger units have higher δ18O ratios and lower 87Sr/86Sr, 206Pb/204Pb, and 207Pb/204Pb ratios with time as the magmatic system rebounds to “normal” Yellowstone rhyolite compositions following caldera collapse. An example of 206Pb/204Pb versus δ18O ratios is presented in Figure 10.

Figure 9. 87Sr/86Sr ratios versus age in millions of years. The horizontal shaded area represents "normal Yellowstone" ratios.

Following the two major eruptions there was an increase in radiogenic Sr preserved in rhyolites. Note that the extra-caldera mingled magmas contain elevated Sr ratios due to mixing with basalt. Data compiled from Hildreth et al. (1984 and 1991),

Christiansen (2001), Bindeman and Valley (2001), Nastanski (2002) Christiansen et al. (2007) and this study.

Figure 10. 206Pb/204Pb ratios versus δ 18O ratios. Analyses from this study presented in elongated boxes, extents represent variability in analyses. DRF - Dunraven Road flow; SILVER - Silver Cord flow, Canyon flow, and TSC - Tuff of Sulphur Creek.

MBBF, NBBF, and SBBF – Middle, North, and South Biscuit Basin flows (Doe et al., 1982; Bindeman et al., 2008) are plotted for comparison. General values from other Yellowstone rhyolites presented in box. Generally, the UBM rhyolites trend towards the “normal Yellowstone” signature with time.

EC-RAxFC Models

A major contribution of this research is a model of the Yellowstone Plateau rhyolites using energy constrained, recharge, assimilation, and fractional crystallization model (EC-RAxFC), as presented by Spera and Bohrson (2002) and Bohrson and Spera (2003). Model results used for this section and Chapter 3 are presented in Appendix B. This model of crustal assimilation and melting generally agrees with observations by McCurry et al. (2008), Watts et al. (2010), and Boroughs et al.

(2005) for rhyolites in the Snake River-Yellowstone track where rhyolites are generated from a felsic crustal source and heat sourced from mafic intrusions. Figure 11, presents the results from models using

EC-RAxFC. Simple mixing models require elevating concentrations of Sr and Nd in the crustal end member to unrealistic levels, e.g. 500 ppm, or decreasing concentrations in the basaltic end member to orders of magnitudes less, e.g. 20 ppm. However, EC-RAxFC models generate realistic curves for the rhyolites using measured data.

Models A and B are based on a mixture of Junction Butte basalt (Hildreth et al., 1984) and

Archean basement (Lamar Canyon – sample 08CP61), with recharging magmas that are equivalent to

Junction Butte basalt. Both Junction Butte basalt and Swan Lake basalt values are used for Models C as the initial magma composition, results were similar with either basalt. Model D uses Swan Lake basalt for the initial magma composition as the rocks being modeled were relatively younger extra-caldera rhyolites. Models using either basalt or an average Yellowstone basalt yielded similar results.

Variables used in the models include: initial basaltic temperature of 1184oC, calculated using

MELTS (Ghiorso and Sack, 1995), initial wall rock temperature of 450oC (using lower wall rock temperatures for Model A did not substantially change the model), magma solidus of 750oC, and assimilant liquidus of 1129 oC (estimated from MELTS and assumed to be lower than the magmatic temperatures for EUBM). Model curves are presented in Figure 11, where Models A and B, and C and D use the initial variables as described above with the exception of equilibration temperatures (Teq)/ Mass of

o assimilated wall rock (Mao). Teq / Mao values for each model are: Model A 894.03 C / 2.091, Model B

910.05oC / 1.848, Model C Junction Butte basalt - 933.37oC / 1.496 (Swan Lake basalt: 915.88oC / 1.759), and Model D 1025.17oC / 0.970. Tables 3 and 4 present the variables used for each of the models.

During the defense of this dissertation it was pointed out that using one sample from the Beartooth

Mountains may not be sufficient for modeling the wall rock composition. A review of published data for the southern Beartooth Mountains (Wooden and Mueller, 1988; Meen 1987) found the average

87 86 143 144 Sr/ Sr(480ka) equaled 0.72434, standard deviation of 0.0373 and Nd/ Nd equaled 0.510772, standard deviation of 0.0005. Average southern Beartooth Mountain radiogenetic isotopes are similar to the Lamar

87 86 Canyon; however, the Sr/ Sr(480ka) value is slightly less than the Lamar Canyon sample (Figure 11). The average southern Beartooth Mountain radiogenetic isotopes can still be used to model most of the

87 86 rhyolites at Yellowstone, but the Sr/ Sr(480ka) would not allow for modeling of the

Huckleberry Ridge, member C. We prefer to use the Lamar Canyon sample, as values were measured using the same analytical facilities and methods as the units focused on in this study.

Figure 11. Radiogenic Isotope ratios, Nd vs. Sr. Results from five EC-RAxFC models presented as A, B, C, and D. MBBF,

NBBF, and SBBF – Middle, North, and South Biscuit Basin flows, mj – Mount Jackson, bc – Blue Creek flow. Basaltic end members used were SLF – Swan Lake Flat basalt and JB – Junction Butte basalt. Lamar Canyon was the crustal end member used for modeling. Archean granitic-gneiss from Lamar Canyon, Yellowstone was analyzed in this study.

We envision that the initial rhyolites had lower equilibration temperatures due to the cooler wall rock. When the initial magma formed a large, or numerous small, magma chamber(s) a rock type with radiogenic signatures on-par with Model A crystallized around the magma chamber. The magma chamber was most likely subjected to further intrusions, magma mixing, and homogenization, forming the “normal” Yellowstone signature (Model B). Model A may have formed from initially cooler wall rock; however, slight variations in initial wall rock temperature (300 to 500 oC) did not result in major changes to the model results. This crystallized material (Model A) would later be subsided to melting depths during subsequent caldera collapses.

Models C and D represent extra-caldera rhyolites, where extensional faulting may allow for relatively faster ascension rates, thus resulting in smaller Mao values. In Chapter 2 we illustrate how rhyolites, modeled using EC-RAxFC, are affected by mixing with mafic intrusions to form the larger range of 87Sr/86Sr ratios but more confined ranges of 144Nd/143Nd.

Table 3. EC-RAxFC Thermal Parameters for Models (Recharge, enthalpy, and specific heat from Bohrson and Spera (2003)).

Initial Magma (m), Recharge Magma (r), Assimilant (a), liquidus (l).

Model: A B C -JB C-SLF D Pristine Magma 1184 1184 1184 1184 1184 o o Tl,m & T m ( C) Recharge Magma 1184 1184 1184 1184 1184 o o Tl,r & T r ( C) Assimilant liquidus 1129 1129 1129 1129 1129 o Tl,a ( C) Initial Assimilant 450 450 450 450 450 o o T a ( C) Mass of Recharge Magma 0.5 0.5 0.5 0.5 0.5 o Ts ( C) 750 750 750 750 750 o Teq( C) 894.0 910.1 933.4 915.9 940.7 Mao 2.09 1.85 1.5 1.76 1.39

Models also presented results indicating that the transition between mafic and felsic melt was over a small temperature interval, once the temperature of the wall rock came to equilibrium with the temperature of the magma (Figure 12). This observation may indicate why intermediate rocks are not generally found in the Yellowstone Plateau and why basalts would stall in the shallow crust. This topic is further addressed in Chapter 3. Such observations may be related to the equations used to develop the EC-RAxFC model and may require further study for validation in the real world.

Table 4. EC-RAxFC Compositional Parameters for Models

(based on measured data and suggestions from Bohrson and Spera (2003)) Recharge = Initial Magma

Sr Nd o C m JB (ppm) 312 23 o ε m JB 0.706451 0.812385 Dm JB 4 0.4 o C m SLF 419 17 (ppm) o ε m SLF 0.705400 0.512483 Dm SLF 4 0.7 o C a (ppm) 436 38 o ε a 0.728666 0.510803 Da 6 0.6

Figure 12. 87Sr/86Sr versus Temperature (oC) for Model A. Temperature of the assimilant increases as the magma cools, equilibration occurs at the apex. Notice the large range in Sr ratios just prior to equilibration.

Summary of Conclusions From This Dissertation

As discussed in the following two chapters this research has concluded:

1. The oldest members of the EUBM, the Tuff of Uncle Tom’s Trail and Tuff of Sulphur Creek

are most likely the same unit and were deposited from a pyroclastic density current based on

field observations.

2. The Canyon flow is most likely composed of multiple flows, with at least one younger flow

exposed near the Silver Cord Falls area.

3. The youngest rhyolite of the EUBM is most likely an extra-caldera unit similar to the

Roaring Mountain Member and is the only known low-δ18O rhyolite erupted from outside

the caldera boundaries. The formation of the Dunraven Road flow can be best explained by

a single EC-RAxFC event assuming that hydrothermal alteration extended to depths along

the ring fracture zone.

4. Genesis of the Tuff of Sulphur Creek and Canyon flow involved the hydrothermal alteration

of the cooled margins of the larger magma chamber feeding the Yellowstone volcanic area,

modeled using EC-RAxFC, followed by subsidence and remelting following the collapse of

the current caldera.

5. Radiogenic isotope signatures found in some of the extra-caldera rhyolites may be caused by

cryptic magma mixing.

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CHAPTER 2

MIXED MAGMA COMPLEXES AND EXTRA-CALDERA VOLCANISM IN THE NORRIS-MAMMOTH CORRIDOR

Chad J. Pritchard, Peter B. Larson, Terry L. Spell, and Kevin Tarbert

Modified from manuscript submitted to Journal of Volcanology and Geothermal Research

Abstract

Mingling and mixing between rhyolite and basalt magmas is evident in four volcanic units along the Norris-Mammoth Corridor in Yellowstone National Park. The presence of at least four mingled magma complexes suggests that mingling is not due to random intersections of feeder dikes, and radiogenetic isotope modeling suggests that mixing may be more common than previously expected.

Extremities of the mingled units exhibit less mingling than the central portion of the units. Initially, eruptions of mingled complexes were dominated by rhyolite, followed by a partially mixed rhyolite with mingled basalt during the later stages of eruption. The temperature of the rhyolitic magmas was approximately 850oC, and viscosities were between 2 x 106 and 3 x 106 Pas. The basalt was approximately 1070oC with a viscosity of 1 x 102 to 3 x 102 Pas prior to mixing. Yellowstone’s mixed magmas may represent established shallow rhyolitic magmas that pull underlying, isotopically distinct, basaltic magmas into the eruption, or mixing could have occurred due to mafic dikes intruding the rhyolitic magma chamber. Rhyolite genesis may have included assimilation of Archean country rock and fractional crystallization into the initial magma. The presence of mafic enclaves and variable geochemistry suggests that mixed magma complexes did not have enough time, or energy, to thoroughly mix in the conduit. Isotopic ratios are generally more radiogenic for extra-caldera rhyolites than intracaldera rhyolites. A model is presented to explain the radiogenic isotope ratio signature and suggests that other extra-caldera rhyolites may have been subjected to small degrees of rhyolite and basalt mixing.

Introduction

With the exception of the mingled magma complexes volcanic rocks from Yellowstone are either basaltic or rhyolitic. Mingled magma complexes contain both of these volcanic products within the same flow and partial mixing produced intermediate magmas. Understanding how these complexes form may be used to better understand magma genesis and eruption mechanisms for smaller volcanic units.

Yellowstone’s extensional Norris-Mammoth Corridor houses numerous extra-caldera basalts and rhyolites, including at least four mingled magma complexes (Figure 13). Rhyolites that erupted following the most recent caldera collapse, post 640±2 ka (Lanphere et al., 2002), are grouped as the Plateau

Rhyolite. The intracaldera portion of the Plateau Rhyolite are designated as the Upper Basin Member and the Central Plateau Member and erupted over similar times as the mingled magmas (Christiansen and

Blank, 1972; Gansecki et al., 1996; Bindeman and Valley, 2000; Vazquez and Reid, 2002; Girard and

Stix, 2009; Girard and Stix, 2010). The extra-caldera portions of the Plateau Rhyolite are divided into the

Roaring Mountain Member and Obsidian Creek Member (Christiansen and Blank, 1972). Division of the extra-caldera members is based upon petrography, where the Roaring Mountain Member is mostly aphyric and the Obsidian Creek Member contains abundant quartz, sanidine, and plagioclase phenocrysts

(Christiansen and Blank, 1972). The aphyric nature of the Roaring Mountain Member implies that it was emplaced at, or above, the magma liquidus (Christiansen et al., 2007). Units from each member and proximal basalt flows are listed in Table 5. The youngest mingled magma is the Crystal Spring flow is

80±3 ka, based on K-Ar sanidine age estimates (Obradovich, 1992). Other mingled magmas have been measured using 40Ar/39Ar age determinations include: Grizzly Lake = 263±3 ka, Gardiner River = 301±3 ka, and Appolinaris Spring dome = 316±2 ka (Christiansen et al., 2007; Nastanski, 2005). This study focuses on the Grizzly Lake, Gardiner River, and Crystal Spring mingled magma complexes, however, similar mixing has also been documented for Appolinaris Spring dome (Nastanski, 2005). These complexes are located near Basin and Range style normal faults (Christiansen, 2001).

Figure 13. A) Map of Yellowstone National Park showing the three calderas of Yellowstone, most recent resurgent domes, and extra-caldera volcanism. N.M.C. – Norris-Mammoth Corridor. B) Close up of the N.M.C. and the four mingled magma complexes: GL- Grizzly Lake, GR – Gardiner River, CS – Crystal Spring, and AS – Appolinaris

Spring, black lines represent faults. Maps modified from Christiansen (1999 and 2001).

Table 5. Post Lava Creek Tuff, extra-caldera volcanic units from the Norris-Mammoth Corridor Area, modified from

Christiansen (2001) and Pritchard and Larson (in progress).

Roaring Mountain Age* Obsidian Creek Age* Proximal Basalts Age* Member (ka) Member (ka) (ka) Crystal Spring 80±3I Gibbon Hill dome 134±8 VI Basalt of Geode >13,<64 V Creek Obsidian Cliff 106±1 VI Paintpot Hill 208±5 II Falls River basalt >11,<64 V flow dome Gibbon River 118±10 II Landmark dome 226±6 II Swan Lake Flat >32,<64 V basalt Obsidian Cliff 183±3 I Grizzly Lake 263±3 VI Panther Creek 174±46 IV flow vent Cougar Creek 399±3 I Gardiner River 301±3 II Lamar River flow 220±41 I dome Dunraven Road 480±8 III Appolinaris 316±2 II Madison River 530±60 I flow Spring dome basalt Riverside flow 526 ±3 II Willow Park 326±2 II Undine Falls 588±26 I dome basalt * Ages from I) Obradovich (1992), II) Nastanski (2005), III) Gansecki et al. (1996), IV) Bennet (2006), V) Christiansen (2001), and V1) Christiansen et al. (2007).

Geologic Background

Of the mingled magma complexes at Yellowstone, the Gardiner River flow is by far the most well studied. It was originally described by Iddings (1899) and Fenner (1938), but became very well known due to the 1944 Fenner-Wilcox debate in the Geological Society of America Bulletin. Fenner

(1938) described the Gardiner River complex as a rhyolitic flow that picked up basaltic lithics. Wilcox

(1944) interpreted the mingling of the Gardiner River complex as a rhyolitic eruption intruding into a basaltic magma and depicted the Gardiner River complex as a mafic-dominated system, mapped as the

Cataract basalt, with a small portion of intruding rhyolite, the Lodgepole rhyolite. Subsequently,

Christiansen and Blank (1972) mapped the younger Swan Lake Flat basalts where mixed basalt had originally been mapped by Wilcox (1944). Therefore, Gardiner River complex is now considered a rhyolite dominated system, with the upper portions of the outcrops dominated by rhyolite. The complex is likely larger than outcrops exposed by the Gardiner River, as the Swan Lake Flat basalts overlie the complex on both sides of the Gardiner River.

Descriptions of how these magmas mingled have changed through time. Hawkes (1945) compared the descriptions by Fenner (1938 and 1944) and Wilcox (1944) to composite dikes of the “Brito-Icelandic

Province” and questioned if the Gardiner River complex may also be an intrusive “admixture.” However, microphenocrysts in basaltic portions of the Gardiner River and Grizzly Lake complexes are generally well aligned with rhyolitic groundmass, suggesting that both the rhyolite and basaltic magmas were partially liquid when they partially mixed at depth and effused as a single flow (Boyd, 1961; Struhsacker,

1978). Boyd (1961) also described Crystal Spring flow, but interpreted the origin as “a rhyolite that picked up cold pieces of basalt,” which is much different from his findings at the Gardiner River and

Grizzly Lake complexes. A more recent study of the Crystal Spring flow described the petrology and concluded that the flow was indeed a mingled magma complex (Nastanski, 2005).

Field observations indicate that these mingled magma complexes are generally dominated by rhyolite, with basaltic enclaves in greater abundances in the basal portions and centers of the units.

Other mixed or mingled magma complexes have been described at Appolinaris Spring dome

(Nastanski, 2005), the flow front of the Obsidian Cliff flow (Boyd, 1961), and the Geode Creek basalt

(Struhsacker, 1978). We have undertaken detailed mapping of the Grizzly Lake complex, measured major and trace element concentrations, gathered microprobe data from the Grizzly Lake, Gardiner River, and Crystal Spring complexes; as well as radiogenic isotopes from the Crystal Spring flow. Together with data from Nastanski (2005), we evaluate magma genesis and mixing process at Yellowstone primarily using radiogenic isotope ratio models.

Material and Methods

A sampling permit was issued by the Yellowstone National Park for the three summers of sampling. Sample locations were recorded using a hand held GPS unit and topographic maps. We attempted to collect isolated portions of rhyolite and basaltic material, as well as representative mixed and mingled samples. However, in many cases samples of basalt and rhyolite were sub-sampled by cutting samples and also picking fragmented samples.

Samples were analyzed for whole rock major and trace element concentrations (Table 6).

Selected samples were also analyzed using electron microprobe and laser ablation inductively coupled mass spectrometry (LA-ICP-MS) for mineral and glass data (Table 7 and Appendices). Radiogenic isotopes were also measured for the Crystal Spring flow (Table 6 and Appendices). All analyses were conducted in the Washington State University GeoAnalytical Laboratory. Major element concentrations were measured from ground fused beads using a ThermoARL XRF. Trace elements were dissolved and measured using a HP4500 ICP-MS. Glass and mineral analyses for major elements were collected using a JEOL 8500F field emission electron microprobe, with a spot size of 10 microns. Glass and mineral

analyses for trace elements were collected using a New Wave UP-213 laser ablation system and analyzed with a Finnigan Element 2 HR-ICP-MS. Glass and pyroxene analyses were conducted using a 16 micron beam diameter with 72 percent 12-14 J/cm2 at a scan speed of 8 microns/sec. Feldspar analyses were conducted using a 30 micron diameter beam, approximately 12 J/cm2 at a scan speed of 15 microns/sec.

Table 6. Whole rock data from mingled magma complexes

Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Member Creek Creek Creek Creek Creek Creek Creek Creek Creek Gardiner Gardiner Gardiner Gardiner Gardiner Gardiner Gardiner Gardner Gardner Unit River River River River River River River River River Complex Complex Complex Complex Complex Complex Complex Complex Complex northing 4971272 4971272 4971272 4971272 4971343 4971343 4971343 4971113 4971147 Easting 521773 521773 521773 521773 521986 521986 521986 521805 522010 Lithology rhyolitic basaltic rhyolitic basaltic rhyolitic basaltic basaltic Rhyolite rhyolite Age (Ma) 0.300 0.300 0.300 0.300 0.300 0.300 0.300 0.263 0.263 Age error 0.003 0.003 0.003 0.003 0.003 0.003 0.003 0.003 0.003 Sample # GR-1-R GR-1-B GR-2R GR-2-B GR-3-R GR-3B GR-3-2-B 08CP56 08CP57

SiO2 74.12 54.77 76.74 66.24 77.04 64.74 57.33 76.27 76.94 TiO2 0.32 1.39 0.15 0.81 0.13 0.82 1.34 0.170 0.122 Al2O3 12.80 15.39 12.27 14.19 12.13 13.98 15.38 12.52 12.09 FeO* 2.53 9.02 1.58 5.08 1.54 5.63 8.17 1.82 1.74 MnO 0.04 0.14 0.01 0.08 0.01 0.09 0.12 0.040 0.009 MgO 0.61 6.20 0.10 2.30 0.03 3.37 4.83 0.08 0.02 CaO 1.58 8.71 0.56 4.77 0.54 5.11 7.89 0.60 0.51 Na2O 3.63 3.04 3.76 3.55 3.75 3.43 3.35 3.75 3.70 K2O 4.33 1.16 4.81 2.89 4.82 2.73 1.40 4.71 4.85 P2O5 0.04 0.17 0.03 0.10 0.02 0.11 0.17 0.043 0.016 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00

La 66.01 22.17 66.36 49.23 71.34 42.49 41.81 53.94 70.02 Ce 123.41 44.76 114.20 90.04 105.21 82.65 70.01 111.28 121.34 Pr 14.26 5.61 14.55 11.22 15.16 9.78 10.49 12.17 15.04 Nd 52.60 22.92 52.75 42.80 55.85 37.26 40.60 44.46 54.96 Sm 11.47 5.51 11.23 9.63 11.73 8.28 9.32 9.65 11.50 Eu 1.03 1.50 0.91 1.28 0.88 1.21 1.50 0.92 0.88 Gd 11.16 5.71 10.18 9.53 10.47 8.00 8.98 8.74 10.54 Tb 1.89 0.96 1.73 1.64 1.75 1.40 1.53 1.56 1.77 Dy 11.62 5.79 10.30 9.99 10.15 8.55 8.99 9.41 10.40 Ho 2.33 1.14 1.96 1.97 1.91 1.69 1.71 1.88 1.99 Er 6.09 2.96 5.13 5.17 4.89 4.45 4.40 5.10 5.26 Tm 0.87 0.41 0.73 0.73 0.67 0.63 0.62 0.74 0.75 Yb 5.18 2.46 4.32 4.39 3.97 3.82 3.75 4.50 4.42 Lu 0.76 0.36 0.61 0.65 0.57 0.56 0.54 0.66 0.66 Ba 482.65 290.87 496.16 400.00 473.67 366.37 322.95 526 478 Th 18.36 4.20 21.20 12.80 20.13 11.38 6.03 20.00 19.86 Nb 30.60 13.84 33.23 25.55 32.59 22.77 17.08 33.78 33.72 Y 59.63 29.03 46.78 49.35 46.81 42.79 41.46 43.91 49.47 Hf 7.38 3.64 7.79 6.12 7.67 5.56 4.35 7.95 7.92 Ta 2.31 0.94 2.57 1.84 2.53 1.67 1.17 2.54 2.53 U 4.38 1.00 4.21 3.06 3.85 2.64 1.55 4.21 3.71 Pb 24.80 5.98 29.11 21.46 23.96 18.26 13.45 27.66 24.38 Rb 148.54 34.84 168.70 102.56 163.99 93.62 46.61 166.8 168.9 Cs 1.95 0.50 1.97 1.47 1.91 1.52 0.67 1.96 2.04 Sr 79.21 359.22 32.46 203.25 25.43 206.97 316.01 38.49 24.87 Sc 5.09 22.30 2.19 13.50 1.70 12.70 19.27 2.65 2.00 Zr 207.25 121.44 214.00 182.88 205.49 163.08 141.81 227 218

Table 6 (continued)

Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Obsidian Member Creek Creek Creek Creek Creek Creek Creek Creek Gardner Gardner Gardner Grizzly Grizzly Grizzly Grizzly Grizzly Unit River River River Lake Lake Lake Lake Lake Complex Complex Complex Complex Complex Complex Complex Complex northing 4971147 4971147 4971147 4962689 4962689 4962689 4962689 4962689 easting 522010 522010 522010 518948 518948 518948 518948 518948 Lithology spherulite rhyolite basalt rhyolitic basaltic spherulite rhyolitic basaltic Age (Ma) 0.263 0.263 0.263 0.263 0.263 0.263 0.263 0.263 Age error 0.003 0.003 0.003 0.003 0.003 0.003 0.003 0.003 Sample # 08CP57B 08CP58 08CP59 GL-4-R GL-4-B GL-5-L GL-5-R GL-5-B

SiO2 76.99 76.86 65.00 76.62 61.36 77.33 77.39 61.70 TiO2 0.118 0.132 0.819 0.14 1.09 0.10 0.10 1.07 Al2O3 12.39 12.22 14.16 12.19 14.47 12.17 12.05 14.59 FeO* 1.46 1.60 5.60 1.55 6.99 1.35 1.33 6.89 MnO 0.026 0.013 0.083 0.04 0.15 0.03 0.03 0.13 MgO 0.02 0.04 3.02 0.21 4.35 0.03 0.02 4.26 CaO 0.44 0.55 4.95 0.68 6.18 0.30 0.44 6.04 Na2O 3.96 3.77 3.40 3.49 3.51 3.84 3.74 3.50 K2O 4.58 4.79 2.86 5.06 1.78 4.84 4.88 1.67 P2O5 0.018 0.016 0.105 0.02 0.14 0.02 0.01 0.15 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00

La 71.81 70.33 43.69 65.72 52.04 74.15 64.97 46.38 Ce 132.17 130.62 84.61 124.10 93.21 146.63 126.53 94.02 Pr 15.88 15.16 9.95 13.98 12.64 15.99 14.61 11.43 Nd 58.14 55.40 38.08 50.47 48.44 56.40 53.76 43.64 Sm 12.47 11.60 8.38 10.90 10.91 12.21 12.03 9.97 Eu 0.90 0.91 1.24 0.60 1.32 0.43 0.43 1.23 Gd 11.40 10.78 8.32 10.28 10.60 10.66 11.71 9.92 Tb 1.96 1.85 1.42 1.80 1.84 1.93 2.08 1.72 Dy 11.63 11.16 8.64 11.09 11.24 11.64 12.73 10.56 Ho 2.28 2.14 1.71 2.20 2.19 2.24 2.54 2.08 Er 6.08 5.65 4.47 5.89 5.65 5.91 6.86 5.40 Tm 0.86 0.82 0.65 0.86 0.80 0.86 0.98 0.75 Yb 5.20 4.78 3.82 5.17 4.66 5.19 5.99 4.47 Lu 0.75 0.70 0.57 0.75 0.68 0.74 0.88 0.64 Ba 480 492 387 240.62 285.60 106.43 108.57 296.07 Th 20.57 20.17 11.69 21.71 10.25 24.11 23.65 11.30 Nb 34.21 32.08 23.29 33.42 21.61 37.57 37.48 22.12 Y 54.78 54.04 43.62 56.43 56.85 46.80 65.32 52.38 Hf 7.78 7.88 5.69 7.62 5.10 8.15 8.14 5.19 Ta 2.56 2.43 1.72 2.59 1.57 2.86 2.91 1.57 U 4.82 3.70 2.72 5.12 2.43 5.90 5.80 2.41 Pb 28.88 26.04 17.26 32.27 31.90 33.45 34.99 21.33 Rb 166.6 165.4 95.8 187.49 43.95 192.95 195.34 34.51 Cs 3.11 2.05 1.56 3.77 1.10 4.07 4.29 1.04 Sr 23.42 26.40 204.55 22.48 222.14 9.85 10.05 218.06 Sc 1.78 1.91 13.19 2.05 16.80 1.39 1.41 16.52 Zr 209 214 166 191.55 148.83 197.06 196.64 148.36

Table 6 (continued)

Roaring Roaring Roaring Roaring Member Obsidian Creek Obsidian Creek Mountain Mountain Mountain Mountain Grizzly Lake Grizzly Lake Crystal Spring Crystal Spring Crystal Spring Crystal Spring Unit Complex -LCT- Complex flow flow flow flow A northing 4965278 4963487 4965942 4965942 4965942 4965991 easting 519397 519106 522575 522575 522575 522584 Lithology rhyolite basalt basalt obsidian obsidian pumice Age (Ma) 0.263 0.263 0.080 0.080 0.080 0.080 Age error 0.003 0.003 0.002 0.002 0.002 0.002 Sample # GL47 GL51 08CP69B 08CP68 08CP69 08CP70

SiO2 77.91 57.14 58.69 76.58 75.87 76.06 TiO2 0.11 1.31 1.15 0.12 0.16 0.15 Al2O3 11.92 14.96 14.74 12.34 12.43 12.48 FeO* 1.32 8.28 7.68 1.37 1.64 1.59 MnO 0.04 0.16 0.13 0.03 0.03 0.03 MgO 0.04 5.63 5.37 0.22 0.43 0.36 CaO 0.35 7.84 7.51 0.71 0.99 0.83 Na2O 3.39 2.91 3.21 3.76 3.67 3.71 K2O 4.91 1.59 1.37 4.85 4.75 4.77 P2O5 0.01 0.18 0.15 0.01 0.02 0.02 Total 100.00 100.00 100.00 100.00 100.00 100.00

La 43.56 27.97 31.24 60.88 59.69 55.27 Ce 147.12 57.20 64.26 121.49 118.90 113.47 Pr 7.44 6.94 7.89 14.00 13.81 12.35 Nd 24.85 27.50 31.35 51.85 50.96 45.04 Sm 5.31 6.59 7.80 12.33 12.20 10.70 Eu 0.39 1.41 1.17 0.20 0.25 0.23 Gd 5.05 6.50 8.59 12.47 12.34 10.68 Tb 1.01 1.12 1.53 2.28 2.26 1.97 Dy 6.73 6.80 9.64 14.24 14.07 12.30 Ho 1.42 1.34 1.96 2.87 2.82 2.44 Er 4.19 3.52 5.20 7.71 7.54 6.59 Tm 0.67 0.49 0.73 1.13 1.11 0.98 Yb 4.36 2.91 4.30 6.66 6.56 5.96 Lu 0.65 0.43 0.64 0.98 0.96 0.87 Ba 114.71 191.71 126.70 39.39 47.07 46.71 Th 28.06 6.65 10.18 29.16 28.58 29.03 Nb 55.77 18.11 20.53 41.70 39.97 41.11 Y 30.48 33.75 50.90 76.94 74.73 62.20 Hf 7.27 4.36 4.31 7.68 7.61 7.68 Ta 4.09 1.27 1.49 3.22 3.16 3.26 U 6.55 1.49 2.43 6.91 6.77 6.78 Pb 25.73 8.91 38.34 34.73 41.50 32.04 Rb 205.65 47.15 44.87 237.37 231.40 225.78 Cs 3.05 0.75 0.66 5.04 4.86 4.41 Sr 9.29 272.10 236.83 12.15 22.65 18.95 Sc 2.53 21.99 20.33 2.20 2.92 2.76 Zr 179.36 143.33 127.27 162.48 159.82 160.97 206Pb/204Pb 17.17 17.16 207Pb/204Pb 15.56 15.56 208Pb/204Pb 38.34 38.32 143Nd/144Nd 0.512204 0.512204 2 σ error 0.000023 0.000023 87Sr/86Sr 0.705706 0.707701 2 σ error 0.000069 0.000068 δ18O 7.7 (q), 6.2 (p) 7.2 (q), 5.84 (s) * FeO is total iron Major oxides in weight percent and trace elements in parts per million (ppm) Minerals analyzed for δ18O include: (q) – quartz, (p) – plagioclase, and (s) - sanidine

Oxygen isotopic ratios were collected on mineral separates using a laser fluorination vacuum extraction line (Table 6). Gas analyses were measured using a Finnigan Delta S MAT IRMS. Analyses of samples were bracketed by analyses of standards, UWG-2 (Valley et al., 1995) and an in house MM-1 quartz standard. A more detailed description of δ18O ratio measurement techniques are presented in

Takeuchi and Larson (2005). Oxygen isotope ratios are reported in per mil (‰) and are relative to

VSMOW.

Sr and Nd isotopic analyses were conducted on whole rock powders from rhyolite and basalt samples from the Crystal Spring flow (Table 6). Initial column separation was done using AG50W-X8 resin. Second stage column chemistry for Sr separation was conducted using Sr-spec resin. Nd was separated from other REE using HDEHP resin and 0.14 M HCl for loading sample, rinsing resin, and elution. Pb-Pb isotopic analyses were conducted on whole rock powders of basaltic and rhyolitic separates. Pb was eluted using four additions of 6.0 M HCl. All samples for radiogenic isotopic analyses were put into solution with 2 percent HNO3 and measured ratios were collected using a Thermo-Finnigan

Neptune MC-ICP-MS . Ratios for each sample were collected 75 times and averaged, then corrected for mass bias and interferences. Standards used were NBS 987 for Sr, Ames Nd for Nd, and NBS 981 for Pb.

Data are presented in Table 6. See http://www.wsu.edu/~geolab for equipment and analytical information.

Results

Outcrop and Sample Description:

Mingled magma complexes of Yellowstone are all located in the Norris-Mammoth Corridor, north of the Yellowstone caldera (Figure 13). Numerous normal faults have been mapped in this area

(Christiansen, 2001). Units are generally small volume; most outcrops are a maximum of 10 meters high, though basal contacts of these units have not been observed in outcrop. The area of exposed Grizzly

Lake complex is approximately 3 km2, Gardiner River complex is approximately 2 km2, Crystal Spring flow is approximately 0.4 km2, and Appolinaris Spring is approximately 0.2 km2. Generally, outcrops contain more rhyolite at the extremities of the flow. The Grizzly Lake complex is a north-south trending ridge, with outcrops on the east side possibly exposed by faulting, or erosion, giving a partial cross sectional view. Similarly, the Gardiner River complex has been exposed by incision of the Gardiner

River. Each of the units contains enclaves of mafic material. Enclaves typically have abrupt contacts with the surrounding felsic material with some contacts being diffuse and gradational; however, in thin sections contacts commonly appear gradational. Mafic enclaves were often vesicular. Increased vesiculation in the rhyolite was noticed where it was in contact with mafic enclaves, though this was generally towards the centers of the mingled magma complexes.

Based on field observations, the Grizzly Lake complex is approximately 11 percent basalt, 24 percent hybrid material, and 65 percent rhyolite. Mafic enclaves are rounded to angular, from <1cm to approximately 40 cm (Figure 14). Mingled zones are often chaotically banded to swirly, white to grey, highly vesiculated, and contain up to 30% phenocrysts dominated by quartz, plagioclase, alkali feldspar, and trace olivine. Outcrops are generally up to 3 meters wide and 1 meter tall and were exposed mostly on the east side of the ridge. Outcrops at the top of the unit are generally glassy with smaller basaltic enclaves (Figure 14A), whereas outcrops along the east side of the ridge are devitrified, have complex mixing patterns, and contain larger basaltic enclaves (Figure 14B).

A majority of the Grizzly Lake complex outcrops are covered by sediment of variable content with occasional rounded basaltic boulders. Christiansen (2001) published geochemical data from one of these boulders as Basalts of Grizzly Lake (sample 81Y-227C). Analysis of 81Y22-7C compares very well to our sample (GL-29) from a basaltic boulder. Due to the rounded nature of the boulders, presence of plagioclase phenocrysts up to 3 cm in length (which is not observed in the Grizzly Lake complex), and large concentration of TiO2 weight percent, these boulders were most likely part of the glacial sediments

found capping the Grizzly Lake complex. In fact, 2.5 weight percent TiO2 is very high for the

Yellowstone Plateau and is comparable to values presented for the Falls River basalt, which is located south west of the Yellowstone caldera. Though data from these boulders have been published as values for the Grizzly Lake complex, these boulders are not geochemically similar to the mingled magmas.

Figure 14. Photos from the Grizzly Lake complex. A) Upper portion of Grizzly Lake with obsidian hosting basaltic enclaves of variable sizes and rounding. B) Large subangular and small rounded basaltic enclave in a heavily banded to swirly rhyolite/mixed matrix.

Determining percent basalt and rhyolite at the Gardiner River complex is complicated because the outcrops are commonly highly weathered and covered by sediments or the Swan Lake basalts. Wilcox

(1944) considered the bulk of the unit to be basalt, and Nastanski (2005) considered only 25 percent of the outcrop to be rhyolitic. As presented in a compass and tape survey by Fenner (1938) the base of the complex is basaltic with rhyolitic pseudo-dikes, whereas a majority of the unit overlying the basalt is rhyolitic. Based on our observations the lower outcrops contain more mafic material. Platy and blocky structures in outcrops along the banks of the Gardiner River resemble basaltic textures on the weathered surface; however, fresh faces of these rocks are dominated by plagioclase, alkali feldspar, and quartz phenocrysts and are rhyolitic to intermediate in composition. The rhyolitic portion of the Gardiner River appears to be about 35 percent, with a hybrid portion of approximately 45 percent, and a basaltic portion

that is on the order of 20 percent. Basaltic enclaves are rounded to angular and are generally sub- centimeter to 20 cm in size, but can be on the scale of a meter towards the base of the unit.

Table 7. Average feldspar geochemistry of mingled magma complexes

Unit Gardiner River Grizzly Lake Grizzly Lake Crystal Spring Sample Ave 2σ Ave 2σ Ave 2σ Ave 2σ mineral plagioclase alkali feldspar plagioclase plagioclase n 82 18 65 38

SiO2 51.31 2.39 65.77 1.09 51.02 2.04 51.46 1.21

TiO2 0.01 0.07 0.02 0.05

Al2O3 30.30 3.59 19.34 0.70 30.48 1.71 30.68 0.84 FeO 0.65 1.00 0.16 0.13 0.58 0.37 0.67 0.23 MnO 0.01 0.04 0.01 0.04 MgO 0.08 0.62 0.11 0.23 CaO 13.07 1.82 0.55 0.69 13.49 1.38 13.39 0.73

Na2O 4.13 1.06 5.60 0.46 3.82 0.78 3.61 0.46

K2O 0.19 0.41 8.65 1.16 0.13 0.12 0.11 0.06 BaO 0.01 0.06 0.11 0.09 0.02 0.09 0.01 0.03 Total 99.73 100.18 99.68 99.93 n 8 5 10 1 La 0.68 0.14 2.92 3.46 1.01 0.61 2.91 Ce 1.34 0.27 3.19 2.86 2.12 1.36 6.38 Pr 0.12 0.01 0.22 0.23 0.24 0.21 1.01 Nd 0.45 0.06 0.63 0.56 1.21 2.00 3.48 Sm 0.09 0.06 0.14 0.20 0.17 0.14 0.95 Eu 0.27 0.03 1.12 1.02 0.26 0.06 0.34 Gd 0.07 0.07 0.22 0.39 0.17 0.18 0.85 Tb 0.01 0.01 0.03 0.07 0.02 0.02 0.15 Y 0.19 0.14 0.70 1.30 0.48 0.51 3.99 Pb 1.03 0.89 27.61 30.76 5.21 6.12 4.30 Rb 0.44 0.35 98.7 121 0.60 0.44 3.90 Cs 0.02 0.07 0.08 0.11 0.00 0.01 0.11 Sr 523 70.2 133 372 464 85.8 379 Major oxides in weight percent and trace elements in parts per million (ppm) Rhyolitic dikes found in the Gardiner River complex, as described by Fenner (1938 and 1944),

are rhyolite infilling cracks in the underlying basalt, whereas Wilcox (1944) described the complex as

intrusions of rhyolite into a still molten basalt flow. Fenner (1938) describes the pseudo dikes as having

no base in some cases, which is not consistent with descriptions presented by Wilcox (1944) (Fenner,

1944). We interpret the basaltic dominated base as representing a step in the process that led to the

mingled magmas, an upwelling of basalt, which we will discuss later in this paper.

Mafic enclaves in the Crystal Spring flow are very different from the Gardiner River and Grizzly

Lake complexes as they are confined to the base and are only up to 20 cm in diameter. Enclaves comprise approximately 15% of the basal outcrops and are generally elongated, rounded to subangular, and parallel to flow banding. Basal sections of the Crystal Spring flow also contain approximately 40 to

50 percent spherulites in the obsidian portion. The middle portion of the Crystal Spring flow is dominated by obsidian. The upper portion of the unit can be highly vesiculated and are similar to upper breccias found at other lava flows in Yellowstone. Nastanski (2005) describes Appolinaris Spring as consisting of 20 percent mafic enclaves with a small range in size, from 1 cm up to 10 cm.

Whole Rock and Groundmass Geochemistry

Rhyolites from Grizzly Lake, Gardiner River, and Crystal Spring complexes are high silica (>75 weight percent SiO2), which is common in the Yellowstone Plateau (Hildreth et al., 1984) (Table 6).

Extra-caldera basalts along the Norris-Mammoth Corridor are olivine tholeiites (Hildreth et al., 1984).

Major elements measured from the mingled magma complexes generally follow a straight mixing line.

The basaltic portion is very similar to the Swan Lake Flat basalts. The rhyolitic portions are very similar to other extra-caldera rhyolites (Figure 15). Whole rock analyses of mixed and mingled magmas generally span the range between rhyolite and basalt, however, only a few samples plot as dacite. A compositional gap is present between dacite and high-silica rhyolite. As described by Sparks and

Marshall (1986) compositional gaps may be expected when basaltic portions are more fractionated than 4 weight percent MgO. Mixing lines for major elements have been presented by Fenner (1938), Wilcox

(1944), and Nastanski (2005). Figure 16 shows an example of whole rock analyses plotting on a straight mixing line, but micro-scale measurements are highly variable due to the presence of micro-scale- plagioclase crystals.

Petrology

Mineral assemblages are very similar for the rhyolitic portions of Gardiner River, Grizzly Lake, and Appolinaris Spring as the units are part of the Obsidian Creek Member; whereas, Crystal Spring flow is almost aphyric and part of the Roaring Mountain Member of the Plateau Rhyolites. Basaltic portions of each unit are dominated by at least two populations of plagioclase phenocrysts, pyroxenes, and olivine.

Results of phenocryst composition are presented in the Appendix. Mafic and felsic minerals are commonly found in disequilibrium with surrounding phenocrysts and groundmass (e.g. quartz in a mafic dominated groundmass, or olivine in a felsic dominated groundmass). Detailed petrologic investigations of the Gardiner River complex are presented in Fenner (1938), Wilcox (1944), and Stuhsacker (1978). A summary of microprobe analyses conducted during this study are presented in the associated Appendix

We observed up to 25 percent phenocrysts of quartz, alkali feldspar, and plagioclase at the Grizzly Lake and Gardiner River complexes, and trace plagioclase phenocrysts in the Crystal Spring flow.

Figure 15. Total Alkali vs. Silica diagram illustrating the spectrum of rock types present in the Yellowstone mingled magma complexes. Black triangles are measured values from the Yellowstone mingled magma complexes, basaltic and rhyolitic values from the Yellowstone Volcanic Area. Data are from this study, Fenner (1934), Hildreth et al.

(1984), Nastanski (2005).

Quartz phenocrysts from Grizzly Lake, Gardiner River, and Crystal Spring complexes are commonly rounded and can be embayed when surrounded by either rhyolitic or basaltic groundmass.

However, few quartz phenocrysts are present in the Crystal Spring flow. Generally, in mafic groundmass, quartz grains have highly resorbed rims and can also have thin pyroxene coronas. Wilcox (1944) and

Stuhsacker (1978) describe the presence of coronas only when quartz is in a basaltic groundmass.

Alkali feldspars are most common in the Grizzly Lake complex, making up to 10 percent of the rhyolitic portion. Gardiner River complex also contains alkali feldspar, but the Crystal Spring flow only contains trace alkali feldspar. Generally alkali feldspars have a thick (1/4 of the grain thickness) resorption rind, or are extensively resorbed and skeletal. Composition of alkali feldspars from the Grizzly

Lake complex average An3±3 Ab48±4 Or49±6, errors are 2-sigma variation (Table 7, Figure 17A). Values observed are generally more sodium-rich than other sanidines from Yellowstone (Leeman and Phelps,

1981).

Figure 16. Al2O3 and viscosity versus SiO2. Whole rock samples plot as a strain line, where microprobe data has a large spread below approximately 65 weight percent SiO2 due to the presence of micolites. Viscosity is plotted as circles and a regression line is plotted through the viscosity calculations, though the mafic and felsic portions of these complexes are quite different.

Plagioclase phenocrysts from Grizzly Lake average An66±7 Ab34±6 Or1±1 (Table 7, Figure 17A).

Plagioclase phenocrysts associated with the rhyolitic portion generally have the composition An17 Ab71

Or12 and rims are generally resorbed. The Grizzly Lake complex contains plagioclase phenocrysts that are often heavily sieved, which is not as common in the Gardiner River and Crystal Spring complexes.

Plagioclase from the Gardiner River complex average An63±9 Ab36±7 Or1±3 (Figure 17A). Plagioclase from

Crystal Spring flow are dominantly associated with mafic enclaves and average An66±4 Ab33±4 Or1±1

(Figure 17A). Plagioclase therefore are generally labradorite and may be associated with warmer rhyolites or could have originated in the basaltic portions of the melt. Generally, plagioclase phenocrysts do not exhibit consistent chemical variations between cores and rims. Labradorite is generally zoned.

Plagioclase phenocrysts are commonly found as aggregates with pyroxenes and olivine in Grizzly Lake,

Gardiner River, and Crystal Spring complexes. Aggregates are present in felsic and mafic groundmass.

Pyroxene compositions are highly variable in Gardiner River and Grizzly Lake complexes.

Results from microprobe analyses of pyroxenes are presented in Figure 17B and Appendix. Pyroxenes from Gardiner River complex span the solid solution range of augite. As can be seen in Figure 17B, pyroxenes with higher concentrations of Fe generally also have higher concentrations of Ca, when compared to augite. Pyroxenes analyzed in two thin sections from Grizzly Lake grouped as augite. One zoned pyroxene phenocryst also contains a zone of ferro-pigeonite. Ferro-pigonite and ferroaugite are present in other high silica rhyolites from Yellowstone (Hildreth et al., 1984; Sisson, 1991), however, augites are most likely derived from a more mafic magma. Therefore, it is very interesting to find such a continuous solid solution across clinopyroxene concentrations. Thin section observations also indicate the presence of orthopyroxene but in much less abundance than clinopyroxenes, in both the Grizzly Lake and Gardiner River complexes.

Figure 17. Ternary diagrams from mingled magma complexes. A. Feldspar ternary diagram for the mingled magma complexes. B. Pyroxene chemistry for the Gardiner River and Grizzly Lake mixed complexes. Data are presented in the attached Appendix.

Olivine is present in all four of the major mingled magma complexes. Grains are generally small, rounded, and found most commonly in aggregates with plagioclase and pyroxenes, though it can be found as single crystals in felsic or mafic groundmass. Microprobe analysis of 29 grains from the Grizzly Lake complex resulted in an average of Fo80, ranging from Fo82 to Fo78. Eight olivine phenocrysts from Crystal

Spring flow averaged Fo81, ranging from Fo80 to Fo82 (see Appendix). Oxides are also present in mingled magma complexes from Yellowstone.

Anhedral phenocrysts with diffuse boundaries and skeletal textures are present in Gardiner River and Grizzly Lake complexes. Similar phenocrysts from Gardiner River generally had a composition of

An27 Ab67 Or.6. One other extensively resorbed phenocryst was alkali feldspar (An10 Ab66 Or.24) and two possible quartz grains with over 95% SiO2 with minor Al2O3.

Temperatures and Viscosity

Mixed magmas are inherently in disequilibrium. However, using variations of groundmass values from whole rock and glass analyses we found similar temperatures among the different units studied when using the plagioclase-melt geothermometer of Putirka (2008). Temperatures for Grizzly

Lake, Gardiner River, and Crystal Spring complexes were similar. Based on 2-sigma of averages we assume an error of approximately ±10oC. Estimated temperatures for the rhyolitic components are 850oC, and basaltic components were approximately 1070oC. Liquidus temperatures were calculated using

MELTS (Ghiorso, et al., 1995) at 1 kbar, with oxygen fugacities of Q-Fa-Mt for rhyolite, and Ni-NiO for basalt (Hildreth et al., 1984). The liquidus for rhyolite from Grizzly Lake, Gardiner River, and Crystal

Spring was calculated to be approximately 1036 oC. Basaltic portions of the complexes were calculated from the most mafic sample of each flow and results were approximately 1200oC. However, using Swan

Lake Flat basalts as a proxy we calculated similar liquidus temperatures of 1206oC. Using estimated eruptive temperatures and an estimated H2O concentration of 2 weight percent for rhyolite and 1 weight

percent for basalt we calculated the viscosity of the rhyolitic portion to be 1.9 x 106 Pas for the Grizzly

Lake complex, 1.5 x 106 Pas for the Gardiner River complex, and 1.6 x 106 Pas for the Crystal Spring flow, calculations based on Giordano et al. (2008). Basaltic portions of the flows ranged from 280 Pas in the Gardiner River complex to 800 Pas in the Crystal Spring flow. Estimated viscosities of the mingled magmas are presented in Figure 16.

Radiogenic Isotope Ratios

87 86 143 144 Measured radiogenic Sr/ Sr(initial) and Nd/ Nd isotope ratios were similar between the mingled magma complexes and can generally be plotted on the same mixing curve; although, the Crystal

Spring flow has slightly lower 143Nd/144Nd. One exception is a mafic sample from Grizzly Lake, GLM-2a

(Nastanski, 2005), which appears to show signs of crustal contamination with an εNd value of -23, a lower value than other analyses from the Yellowstone Plateau. As illustrated in Figure 18, the rhyolitic portions of the mingled complexes have less radiogenic 87Sr/86Sr ratios than other extra-caldera rhyolites. This may be due to the low concentrations of Sr (ppm) in the rhyolites and cryptic mixing with the less radiogenic basaltic magma. 144Nd/143Nd ratios from rhyolitic portions of mingled magmas generally maintain extra-caldera values (εNd of approximately -12). Mixing models presented are from Bohrson and Spera (2007) for energy constrained- recharge, assimilation, and fractional crystallization (EC-

RAxFC) models (Figure 18A) (Pritchard and Larson, in review).

Radiogenic ratios from the mingled magma complexes plot on the simple mixing curve developed from Gardiner River flow samples. Other extra-caldera rhyolites also plot on the same mixing curve and contain slightly lower 87Sr/86Sr ratios when compared to other extra-caldera rhyolites. Units such as Riverside flow, Landmark dome, and Paintpot Hill dome may have been influenced by minor cryptic mixing with basaltic magmas prior to eruption, after the rhyolites were formed by EC-RAxFC processes. However, there are no descriptions of these units as being mixed magmas, nor has the

presence of basaltic enclaves been published. Therefore, there may be more mingled and mixed units in

Yellowstone, but evidence for mixing has not been observed in the field.

143 144 87 86 Figure 18. Nd/ Nd versus Sr/ Sr(initial) graphs. A. EC-RAxFC models for various volcanic units at

Yellowstone. Beartooth Mountains (Wooden and Mueller, 1988). Yellowstone Basalts, UBM – Upper Basin

Member rhyolites, and bc- Blue Creek flow. Data from: Doe et al., 1982; Hildreth et al., 1991; Bennet, 2006;

Nastanski, 2005; Vazquez et al., 2009; and this study. Models A thru D are EC-RAxFC curves, discussed in text.

B. Close up of the mingled magma complexes. EC-RAxFC model in green, with simple mixing model in blue with crosses every 10% of mixture.

Discussion

Mingled magma complexes at Yellowstone have been described as the result of randomly intersecting feeder dikes of mafic and felsic material resulting in the eruption of mingled volcanic units

(Christiansen, 2001). However, since four documented units exhibit magma mingling and mixing textures, we believe that mixing is more related to magma genesis and structures in the Norris-Mammoth

Corridor than previously thought. Bachman and Bergantz (2004) and many others have presented models where rhyolitic magma bodies, once developed, do not mix well with basalt.

Mingled magmas contain mafic enclaves demonstrate that basalt may not readily mix with rhyolitic magma. Although petrology and chemistry suggests that some mixing has occurred, there is a compositional gap, which has been observed in other mingled or commingled magmas (Sparks and

Marshall, 1986). The mingling process is illustrated in Figure 19 and is also used to describe why the peripheries of the units are dominated by rhyolite and mafic enclaves are generally smaller and have more distinct boundaries towards the surface and extremities of the flows. The presence of quartz and ferrohedenburgite in basalt and olivine, augite, and labradorite in rhyolite also indicates that crystallization had commenced prior to mixing. Using MELTS and mineral phases crystallized prior to mixing and mingling, we estimate that the temperature of the rhyolite was approximately 900oC to 850oC and the basalt at approximately 1000oC, or slightly higher (Ghiorso and Sack, 1995).

Our model for formation of the mingled magmas, therefore, begins with the establishment of a rhyolitic magma body that is under-plated by basaltic intrusion. Pritchard and Larson (in review) have shown that the Dunraven Road flow also contains the radiogenic isotopic signature of extra-caldera rhyolites, although it is a low-δ18O ring fracture dome. This finding suggests that rhyolite genesis occurs in the shallow crust either from melting of the crust, or by assimilation and fractional crystallization processes.

Dome and possibly small lava flow eruptions are most likely initiated in part by degassing of the magma, thereby decreasing the density of the magma and increasing the viscosity, especially in the upper parts of the conduit, as described by Sparks (1997). Grizzly Lake complex serves as a good example, where the upper sections tend to be vitrophyre with low vesiculation and the center of the unit contains high amounts of banding and vesiculation, especially when in contact with basaltic enclaves.

Mingled magma complexes in Yellowstone are located in a structurally extensional area, which is similar to other mingled magma complexes in Iceland and Scotland (Hawkes, 1945), but may not be the case with all mingled magma complexes in the world. We believe that initial build up of pressure in the magma due to degassing is resisted by the surrounding wall rock, however the presence of extensional features may 1) allow for a zone of weakness to allow a rapid release of gas from the upper portion of the rhyolite, or 2) allows for rapid emplacement of basaltic intrusions that can rapidly heat up the rhyolite and increase volatile concentrations by degassing the rhyolite, or adding volutes from the basalt, or 3) a combination of both. Extensional structures may act as path ways to allow for an initial eruption of rhyolite followed, or coeval with, the basalt. Thus, the rhyolite incorporated the upwelling basalt. During ascension the lower portion of the units may retain enough heat to allow entrainment of basalt followed by inflation of the unit to produce a mingled complex with higher proportions of basalt towards the center of the unit. This model for mixing and mingling is conceptually very similar to mixing models presented by Koutchi and Sunagawa (1985) and Bergantz and Breidenthal (2001), however, in the Yellowstone system the rhyolitic magma chambers may be relatively shallow, have lower volatile concentration, are warmer than in arc volcanoes, and mix with mafic magmas. Complete hybridization of magmas requires the mixing of magmas with intermediate chemistry, or more than 4 weight percent MgO (Sparks and

Marshall, 1986) and may indicate that magmas mingled prior to eruption as well. From our models it may be inferred that mingled magma complexes may be more common in Yellowstone than previously

expected, as lower portions of flows and conduits are not generally exposed in the younger rocks, and older units could have easily been blanketed by the voluminous amounts of younger volcanic rocks from

Yellowstone.

Figure 19. Conceptual model for the development of mingled magma complexes at Yellowstone, not to scale, lighter color (pink) is rhyolite and darker portion (gray) is basalt, and mixed portions denoted by small basaltic enclaves.

A. established rhyolite magma chamber is under plated by basaltic intrusions underlying a normal fault. B.

Rhyolite erupts through an established conduit and the underlying basalt is pulled into the eruption. C. As the rhyolite flow inflates basaltic enclaves are pulled into the base of the unit and the unit is partially mixed. Post emplacement erosion and river incision exposes the basaltic base as found in the Gardiner River and Crystal Spring complexes.

Acknowledgments

Sample analyses were conducted at Washington State University GeoAnalytical Laboratories with help from Dr. Rick Conrey, Charles Knaack, Dr. Garret Hart, and Dr. Jeffery Vervoort. Sampling permits were issued by Yellowstone National Park, Research Permit Office, with help from Christie L.

Hendrix. This study was funded by National Science Foundation grant #EAR-0609475, awarded to Dr.

Peter B. Larson, the Washington State University Graduate School, and by the School of Earth and

Environmental Sciences, Washington State University.

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CHAPTER 3

EVOLUTION OF THE UPPER BASIN MEMBER OF THE PLATEAU RHYOLITES

Chad J. Pritchard and Peter B. Larson

Modified from manuscript submitted to Contributions to Mineralogy and Petrology

Abstract

An array of samples from the eastern Upper Basin Member of the Plateau Rhyolite (EUBM) in the Yellowstone Plateau, Wyoming, were collected and analyzed to evaluate styles of deposition, geochemical variation, and plausible sources for low-δ18O rhyolites. Similar depositional styles and geochemistry suggest that the Tuff of Sulphur Creek and Tuff of Uncle Tom’s Trail were both deposited from pyroclastic density currents and are most likely part of the same unit. The middle unit of the

EUBM, the Canyon flow, may be composed of multiple flows based on a wide range of Pb isotopic ratios

(e.g., 206Pb/204Pb ranges from 17.54 to 17.86). The youngest EUBM, the Dunraven Road flow, appears to be a ring fracture dome and contains isotopic ratios and sparse phenocrysts that are similar to extra- caldera rhyolites of the younger Roaring Mountain Member. Petrologic textures, increased radiogenic

87Sr/86Sr in plagioclase phenocrysts (0.7134 to 0.7185) than groundmass and whole rock ratios (0.7099 to

0.7161), and δ18O depletions on the order of 5‰ found in the Tuff of Sulphur Creek and Canyon flow indicate at least a two-stage petrogenesis involving assimilation and fractional crystallization processes.

The presence of a low-δ18O extra-caldera rhyolite indicates that country rock may have been hydrothermally altered at depth and then assimilated to form the Dunraven Road flow.

Introduction

The eastern Upper Basin Member of the Plateau Rhyolite (EUBM) consists of the Tuff of Uncle

Tom’s Trail, the Tuff of Sulphur Creek, the Canyon flow, and the Dunraven Road flow, from oldest to youngest (Christiansen, 2001). Of particular interest is the low-δ18O nature of the EUBM magmas and

increased 87Sr/86Sr, 206Pb/204Pb, and 207Pb/204Pb ratios when compared to other Yellowstone rhyolites

(Hildreth et al., 1991). These units were first documented as low-δ18O rhyolites by Friedman et al.

(1976). The connection between low-δ18O and increased 87Sr/86Sr, 206Pb/204Pb, and 207Pb/204Pb radiogenic isotope ratios was described by Hildreth et al. (1991). Variations in radiogenic isotope ratios following a caldera collapse may be explained by either assimilation of wall rock or magma mixing. However, determining the processes that lead to δ18O ratio depletions in Yellowstone rhyolites has lead to multiple and often contradictory hypotheses. For example, Friedman et al. (1976) in their original description of the δ18O values proposed that magmas absorbed ambient low-δ18O meteoric groundwater to produce the rhyolitic low O ratio signatures, although Taylor (1986) has demonstrated the physical problems with this model. More recent workers favor the involvement of low-δ18O hydrothermally altered rocks as a significant component of the magmas, either by incorporation of altered roof rocks (Hildreth et al, 1984;

Hildreth et al., 1991), or by subsidence of hydrothermally altered volcanic rocks to melting depths

(Bindeman and Valley, 2001).

This study of the EUBM was initiated to measure geochemical variations within each of the rhyolites, and to compare them with other rhyolites from Yellowstone. Variations within individual rhyolite eruptions can be used to better define characteristics of the magmatic feeding system that produced the Yellowstone Plateau Rhyolite. Here, evidence is provided that suggests that the Tuff of

Uncle Tom’s Trail and the Tuff of Sulphur Creek are portions of the same unit, the Canyon flow may be comprised of multiple rhyolites, and that the Dunraven Road flow is more geochemically akin to an extra- caldera rhyolite. This paper also proposes that Energy-Constrained Recharge, Assimilation, and

Fractional Crystallization models (EC-RAxFC) may best explain radiogenic isotope variation and the high-silica values found in the EUBM. If EC-RAxFC processes significantly contribute to rhyolite genesis at Yellowstone then there may be important implications for interpretation of caldera uplift rates and geophysical studies of the area. Current models for rhyolite genesis at the Yellowstone caldera

require significant volumes of basaltic intrusions to partially melt the crust, on the order of equal proportions of basalt to the melted rhyolite (Bindeman et al., 2008). Modeling rhyolite genesis at

Yellowstone using partial melting would predict higher uplift rates than may be required to develop significant quantities of high-silica rhyolites by EC-RAxFC processes.

Figure 20. Map of Yellowstone Volcanic Area, showing approximate locations of the three calderas, extent of Plateau Rhyolite:

Upper Basin Member, Central Plateau Member, and northern extra-caldera rhyolites. Upper Basin Member has been broken into two groups, western and eastern. Map modified from Gansecki et al. (1996) and Christiansen (2001).

Pre-Yellowstone Caldera Geologic History

The Yellowstone caldera is located in northwestern Wyoming, at the easternmost extension of the

Snake River-Yellowstone volcanic track (Christensen, 2001). Basement rocks that are exposed around the caldera include Archean granitoids and biotite schists, Paleozoic and younger shallow marine

sedimentary rocks, and Eocene Absaroka igneous rocks (Christiansen, 2001). These lithologies are potential contributors to the younger rhyolitic magmas.

The southern Beartooth Mountains, located just north of Yellowstone Park, are comprised of

Archean granodiorite, granite to granodiorite gneiss, andesitic amphibolite, and granite biotite schist. U-

Pb measurements of zircon grains and whole rock Pb ratios have been used to estimate the age of the

Archean Beartooth Mountains at approximately 2.8 Ga. This Archean block, which here is considered to represent Archean rocks at depth beneath the caldera, was uplifted during the Laramide orogeny (Wooden and Mueller, 1988). Granitic gneiss, garnet-biotite schist, norite, and migmatite are exposed in the northern portion of the park (Christiansen, 2001).

The Mississippian Madison Limestone outcrops extensively in the northeastern corner of the park and to the south of the caldera, although other sedimentary units have been mapped, for example the

Mississippian Lodgepole Limestone, Devonian Three Forks and Jefferson clastic Formations, Ordovician

Bighorn Dolomite and older Cambrian sedimentary units (Love and Keefer, 1975; Prostka et.al., 1975;

Christiansen, 2001). The presence of deeper sedimentary bedrock outside of the caldera ring fracture zone is suggested by hydrocarbons in the Washburn Hot Springs (Fournier, 1989) and by CO2 emissions

(Werner and Brantley, 2003).

Uncle Tom’s Trail (Christiansen, 2001). Finally, Basin and Range tectonics extends through the park and is present along much of the Snake River-Yellowstone Track, though volcanic rocks associated with the track are not generally faulted (Leeman et al., 2008).

Yellowstone volcanic background

Volcanism from the Yellowstone Plateau produced at least three periods of large-volume caldera- forming eruptions with the first approximately 2.059 ± 0.004 Ma and the latest at approximately 640 ±2 ka based on 40Ar-39Ar measurements (Lanphere et al., 2002). The three caldera-forming eruptions deposited, from oldest to youngest: Huckleberry Ridge Tuff (HRT), Mesa Falls Tuff (MFT), and the Lava

Creek Tuff (LCT). HRT was deposited by at least three eruptions that were the largest known eruptions in the Yellowstone area (Christiansen, 2001). Of the three HRT members, the youngest, member C

(HRT-C) has a substantially smaller estimated initial erupted volume (Christiansen, 2001) and also has a unique radiogenic isotopic signature (Doe et al., 1982; Hildreth et al., 1991). The complex history of precaldera and post-caldera collapse volcanism involves the eruption of basalt and rhyolite on the

Yellowstone Plateau. Following the deposition of the youngest caldera-forming eruption of the LCT numerous basalts and rhyolites erupted outside of the caldera (extra-caldera), and numerous rhyolites erupted from within the caldera (intracaldera). Post-LCT rhyolites are grouped into the Plateau Rhyolite as defined by Christiansen and Blank (1972). 40Ar-39Ar measurements of extra-caldera basalts and rhyolites have yielded ages from 590 ka to 80 ka (Bennett, 2002; Nastanski, 2002; Christiansen et al.,

2007). Ages of the younger intracaldera Central Plateau Member of the Plateau Rhyolite were measured using 238U-230Th and range between 166 ka and 70 ka (Vazquez and Reid, 2002; Vazquez et al., 2009) and

40Ar/39Ar ages estimates between 159 ka and 60 ka (Dallegge, 2008; Simon et al, 2008). The oldest of the intracaldera rhyolites, the Upper Basin Member, are approximately 480 ka to 255 ka, based on 40Ar-39Ar measurements (Gansecki et al., 1996; Bindeman et al., 2008).

The Upper Basin Member has been subdivided into the eastern Upper Basin rhyolites (EUBM), including the Tuff of Uncle Tom’s Trail, Tuff of Sulphur Creek (479 ± 10 ka), Canyon flow (484 ± 15 ka), the

Dunraven Road flow (486 ± 42 ka), and the western Upper Basin rhyolites (WUBM) including the

Biscuit Basin flows and Scaup Lake flow (Gansecki et al., 1996). The Biscuit Basin flows have been

subdivided into the north, south (255 ± 11ka), middle (516 ± 7 ka), and east flows (Gansecki et al., 1996;

Bindeman and Valley, 2001; Bindeman et al., 2008; Girard and Stix, 2009). The Scaup Lake flow is the youngest WUBM rhyolite, 257 ± 13 ka, and is located south of the Biscuit Basin Flows (Christiansen et al., 2007). The older Upper Basin Member (UBM) rhyolites and Blue Creek flow (post –HRT) are the first known intracaldera rhyolites that followed caldera collapse and have up to 5‰ depletion in δ18O values with slightly elevated Sr and Pb isotope signatures (Hildreth, 1984; Bindeman and Valley, 2001).

The Mesa Falls Tuff, Lava Creek Tuff and the Central Plateau Member are also slightly low in δ18O values, with depletions in quartz up to 2‰ when compared to “normal Yellowstone rhyolites” (Hildreth et al., 1984; Bindeman et al., 2008).

The Upper Basin Member exhibits an age progression in δ18O values where the older units such as Middle Biscuit Basin flow and Tuff of Sulphur Creek/Canyon flow show larger δ18O depletions and younger units such as south Biscuit Basin flow and Scaup Lake show less of a δ18O depletion (Gansecki et al, 1996; Bindeman et al, 2008). One exception to this trend is the less δ18O depleted Dunraven Road flow, although as noted in this paper, this flow is geochemically distinct from the other UBM units.

EUBM are located within, and straddling, the northeastern caldera margin and are north of the

Sour Creek resurgent Dome (Figure 20). Generally, these flows contain up to 35% phenocrysts

(Christiansen 2001). However, the youngest of the EUBM, the Dunraven Road flow, contains fewer phenocrysts, 8% or less, which differs from other Upper Basin Member rhyolites (Girard and Stix, 2009).

Previous studies describe the Tuff of Uncle Tom’s Trail as deposited from pyroclastic density currents, the Tuff of Sulphur Creek as an agglutinated ash fall tuff, and the younger units as rhyolitic lava flows (Christiansen and Blank, 1972; Girard and Stix, 2009). Geochemical studies of these units have concluded that many of the flows are from isolated magma bodies (Girard and Stix, 2009), whereas the next series of flows, the Central Plateau Member of the Plateau Rhyolite, are thought to have erupted from a single large magma body located within the caldera (Vazquez et al., 2009). These studies

generally agree with a model of silicic magma genesis presented by Huppert and Sparks (1988), where basaltic intrusions melt or assimilate crustal material in small batches which coalesce into a single large magma chamber over time. This study presents new radiogenic isotope values for whole rock and separated glass for a majority of the UBM rhyolites, including the North, South, and East Biscuit Basin flows and the Dunraven Road flow, and presents a model for the petrogenesis of the EUBM.

Sampling and Methods

A sampling permit was issued by the National Park for the three summers of sampling. Each sample was located using a hand held Garmin GPS unit, sample locations are listed in the Appendix

(whole rock data). Glass separates were picked using a specimen microscope from chipped and sieved

(500 micron) vitric hand samples to ensure the purest possible sample. However, microphenocrysts may be present in samples even though microphenocrysts were not commonly observed in thin section.

Analytical data were collected in the Washington State University GeoAnalytical Laboratory.

Major element concentrations were measured from ground fused beads using a ThermoARL XRF

(Tables 8 and 9, Appendix). Trace elements were measured using a HP4500 ICP-MS (Tables 8 and 9,

Appendix). Glass and mineral analyses for major elements were collected using a JEOL 8500F field emission electron microprobe with a spot size of 10 microns (Table 9, Appendix). Glass and mineral trace element data were collected using a New Wave UP-213 laser ablation system and analyzed with a

Finnigan Element 2 HR-inductively coupled plasma mass spectrometer (LA-ICP-MS), results are presented in Table 10 and the Appendix. Glass and pyroxene analyses were conducted using a 16 micron beam with 72% 12-14 J/cm2 at a scan speed of 8 microns/sec. Feldspar analyses were conducted using a

30 micron beam, approximately 12 J/cm2 at a scan speed of 15 microns/sec. Background levels in the vacuum sample holder were collected for 10 seconds and used for corrections, standards NBS612 and

BCR were routinely run for calibration purposes.

Oxygen isotopic ratios were collected on mineral separates using a laser fluorination vacuum extraction line. Gas analyses were measured using a Finnigan Delta S MAT IRMS. Analyses of samples were bracketed by analyses of standards, UWG-2 (Valley et al., 1995) and an in house MM-1 quartz standard. A more detailed description of O ratio measurement techniques are presented in Takeuchi and

Larson (2005). Oxygen isotope ratios are reported in per mil (‰) and are relative to VSMOW.

Sr and Nd isotopic ratio analyses were conducted on whole rock powders and glass separates

(Table 9). Samples were dissolved in H3BO3 and twice with 6.0 M HCl, in clean Teflon crucibles.

Samples were then dissolved in 6 M HCl and H2O for column chemistry. Initial column separation was done using AG50W-X8 resin, with a series of washes using 2.5 M HCl and 6.0 M HCl. First stage Sr elution was conducted using 2.5 M HCl and REEs (Nd) were separated using 6.0 M HCl. Samples were dried down and treated with 14 M twice distilled HNO3 to remove organic residue from resin. Second stage column chemistry for Sr separation was conducted using Sr-spec resin. We used 3 M HNO3 to load sample and to rinse resin and then 0.5 M HNO3 to rinse resin and elute Sr. Nd was separated from other

REE using HDEHP resin and 0.14 M HCl for loading sample, rinsing resin, and elution. Samples were dried down and treated with 14 M twice distilled HNO3 to remove organic residue from resin.

Pb isotope analyses were conducted on whole rock powders and glass separates (Table 9).

Sample dissolution involved fluxing with HF and HNO3 (10:1), drying down, and fluxing with 8 M HBr in Savillex crucibles. Samples were then dissolved in 0.5 M HBr to load into columns, with AG1-X8 resin. Columns were repeatedly rinsed with H2O, 0.5 HBr, 1.0 M HCl, and 6.0 M HCl. Pb was eluted using four additions of 6.0 M HCl. All samples for radiogenic isotopic analyses were put into solution with 2% HNO3 and measured ratios were collected using a Thermo-Finnigan Neptune MC-ICP-MS.

Ratios for each sample were collected 75 times and averaged, then corrected for mass bias and interferences. Standards used were NBS 987 for Sr, Ames Nd for Nd and NBS 981 for Pb.

Table 8. Average whole rock analyses of EUBM.

Tuff of Sulphur Dunraven Road Unit Creek Canyon flow flow n = 23 2σ n = 29 2σ n = 12 2σ XRF (weight percent) SiO2 76.45 1.25 76.10 1.31 77.46 0.45 TiO2 0.34 0.04 0.32 0.12 0.12 0.02 Al2O3 12.6 0.38 12.6 0.61 12.2 0.31 FeO* 1.54 0.96 1.80 0.58 1.13 0.23 MnO 0.03 0.02 0.04 0.04 0.02 0.02 MgO 0.06 0.06 0.09 0.12 0.04 0.03 CaO 0.66 0.21 0.75 0.42 0.44 0.15 Na2O 3.34 0.25 3.27 0.81 3.46 0.05 K2O 4.99 0.25 4.98 0.54 5.16 0.06 P2O5 0.03 0.01 0.03 0.02 0.02 0.01 Total 100 100 100 ICP-MS (ppm) La 78.1 17.9 76.5 10.75 58.9 16.9 Ce 149 41.2 146 24.0 117 45.3 Pr 17.3 4.45 16.9 2.80 12.8 4.00 Nd 62.8 16.1 61.4 12.2 45.8 15.0 Sm 12.9 3.28 12.7 3.28 9.60 3.08 Eu 1.92 0.37 1.94 1.15 0.72 0.09 Gd 11.6 3.16 11.7 5.22 8.59 2.76 Tb 1.97 0.53 1.99 0.93 1.49 0.43 Cy 11.9 3.06 12.1 5.96 9.13 2.48 Ho 2.35 0.62 2.43 1.32 1.80 0.47 Er 6.34 1.58 6.59 3.60 4.88 1.20 Tm 0.92 0.23 0.95 0.48 0.71 0.16 Yb 5.63 1.40 5.87 2.68 4.43 0.94 Lu 0.86 0.22 0.89 0.41 0.66 0.15 Ba 1019 132 1016 205 673 35 Th 24.1 1.56 23.1 1.86 20.9 1.57 Nb 49.3 1.88 46.6 6.81 33.6 1.69 Y 57.9 17.6 61.5 42.89 46.0 13.7 Hf 10.8 0.68 10.4 2.18 7.05 0.40 Ta 3.45 0.16 3.28 0.39 2.50 0.12 U 5.95 0.62 5.69 0.69 4.53 0.38 Pb 31.9 12.67 30.1 3.96 31.1 6.20 Rb 173 12.3 170 21.9 170 4.3 Cs 3.41 1.36 3.72 1.95 2.98 1.19 Sr 73.3 21.81 76.4 42.12 20.1 5.19 Sc 5.80 1.72 5.78 2.12 4.00 0.89 Zr 369 40.6 354 108.0 194 14.1

Table 9. Major and trace elements and radiogenic isotope ratios for UBM

Upper Upper Upper Upper Upper Upper Upper Upper Member Basin Basin Basin Basin Basin Basin Basin Basin Unit TSC TSC CAN CAN CAN DRF DRF DRF northing 4956461 4956400 4951810 4952622 4949551 4955387 4955840 4955642 easting (12) 547171 547245 542014 543804 555907 540434 542283 542334 picked picked picked Lithology vitric vitric tuff obsidian tuff glass glass glass Age (Ma) 0.479 0.479 0.484 0.484 0.484 0.486 0.486 0.486 Age error 0.01 0.01 0.015 0.015 0.015 0.042 0.042 0.042 Sample # 08CP12 0835G* 08CP26 0822 0934G* 07CP15 08CP01 0921 XRF (weight percent) SiO2 76.24 77.76 76.55 75.99 77.15 77.59 77.34 77.57 TiO2 0.38 0.24 0.34 0.31 0.25 0.12 0.13 0.12 Al2O3 13.12 11.95 12.64 12.45 12.00 12.17 12.09 12.10 FeO* 0.83 1.10 1.35 2.08 1.41 0.88 1.18 1.22 MnO 0.02 0.03 0.03 0.06 0.04 0.02 0.03 0.01 MgO 0.18 0.06 0.07 0.14 0.09 0.04 0.07 0.01 CaO 0.98 0.38 0.83 0.72 0.49 0.47 0.53 0.37 Na2O 3.55 2.68 2.50 3.42 3.18 3.48 3.49 3.44 K2O 4.67 5.78 5.65 4.80 5.37 5.20 5.13 5.15 P2O5 0.02 0.02 0.02 0.03 0.02 0.02 0.01 0.01 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 99.33 97.30 96.17 99.44 91.57 96.73 98.88 97.55 ICP-MS (ppm) La 72.76 74.24 78.43 71.87 76.22 60.39 62.52 37.26 Ce 136.01 142.15 150.32 138.93 148.25 111.95 119.12 72.50 Pr 16.01 15.79 17.00 15.63 16.74 12.80 13.39 7.66 Nd 57.86 55.88 61.35 56.17 60.19 45.68 48.38 26.93 Sm 11.98 11.16 12.65 11.50 12.37 9.49 10.15 5.72 Eu 2.31 0.83 1.91 1.73 1.12 0.69 0.72 0.69 Gd 10.41 10.52 11.63 10.57 11.14 8.78 9.32 5.11 Tb 1.74 1.79 1.96 1.81 1.95 1.50 1.58 0.93 Cy 10.67 11.07 12.12 11.20 11.81 9.19 9.71 5.70 Ho 2.12 2.23 2.44 2.28 2.36 1.82 1.95 1.16 Er 5.68 6.10 6.86 6.24 6.52 4.92 5.33 3.21 Tm 0.84 0.89 0.99 0.91 0.93 0.72 0.76 0.49 Yb 5.15 5.53 6.17 5.72 5.85 4.35 4.77 3.11 Lu 0.79 0.87 0.95 0.87 0.89 0.66 0.72 0.46 Ba 1163 677 1034 1016 698 671 664 656 Th 22.36 25.14 23.56 21.77 24.62 23.07 20.14 20.39 Nb 46.05 48.59 48.45 42.97 48.12 34.24 33.45 33.75 Y 53.10 58.12 63.83 58.82 62.45 47.02 51.20 27.03 Hf 11.60 8.67 10.75 9.53 8.68 7.06 7.06 6.79 Ta 3.24 3.53 3.41 3.05 3.42 2.54 2.50 2.50 U 5.68 6.06 5.85 5.51 6.01 4.67 4.53 4.35 Pb 25.37 32.02 30.86 31.90 30.10 32.10 31.44 28.49 Rb 152.0 235.0 186.6 162.7 174.0 172.4 172.2 167.3 Cs 3.73 5.05 5.94 4.11 4.04 3.27 3.38 1.84 Sr 110.49 26 83.05 78.47 27 19.28 20.14 20.31 Sc 6.46 4.8 5.74 5.39 5.1 3.44 4.00 3.91 Zr 404.2 285.5 372.3 318.3 282.9 191.5 190.7 195.1 206Pb/204Pb 17.78 17.84 17.81 17.54 17.86 16.68 16.67 16.68 207Pb/204Pb 15.64 15.65 15.65 15.59 15.65 15.45 15.44 15.45 208Pb/204Pb 38.36 38.4 38.37 38.23 38.40 37.79 37.77 37.81 87Sr/86Srm 0.71569 0.71575 0.71597 0.71605 0.71318 0.71334 2 σ error 0.00005 0.00007 0.00004 0.00007 0.00004 0.00007 143Nd/144Nd 0.512152 0.512181 0.512163 0.512224 0.512177 0.511965 0.511976 0.511982 2 σ error 0.000029 0.000023 0.000012 0.000023 0.000023 0.000029 0.000012 0.000023 epsilon Nd -9.5 -8.9 -9.3 -8.1 -9.0 -13.1 -12.9 -12.8

Table 9 (continued)

Member Upper Basin Upper Basin Upper Basin Precambrian Unit SBBF NBBF EBBF bedrock northing 4925596 4931015 4924479 4973680 easting (12) 510161 486037 487852 556305 Lithology picked glass picked glass picked glass granitic-gneiss Age (Ma) 0.255 0.2? 0.5? 2.8 Age error 0.011 0.05 Sample # YC96-2G** 08YS-14BG** 08YS-15BG** 08CP061 XRF (weight percent) SiO2 77.41 75.42 65.66 TiO2 0.19 0.34 0.86 Al2O3 12.15 12.36 15.84 FeO* 1.09 2.29 5.05 MnO 0.03 0.05 0.07 MgO 0.08 0.19 1.52 CaO 0.41 0.84 3.98 Na2O 3.18 3.34 3.98 K2O 5.43 5.11 2.76 P2O5 0.01 0.05 0.28 Total 100.00 100.00 100.00 Raw Sum 96.01 91.81 98.35 ICP-MS (ppm) La 76.22 38.62 72.77 39.04 Ce 138.32 66.78 140.27 86.69 Pr 15.61 7.57 15.69 10.25 Nd 53.78 25.78 55.68 38.32 Sm 10.53 5.17 11.49 6.99 Eu 0.87 0.30 1.31 2.02 Gd 9.07 4.26 10.31 5.55 Tb 1.55 0.78 1.82 0.70 Cy 9.50 4.84 10.75 3.78 Ho 1.92 0.96 2.22 0.70 Er 5.20 2.58 6.00 1.79 Tm 0.76 0.39 0.87 0.25 Yb 4.75 2.41 5.40 1.54 Lu 0.73 0.36 0.83 0.25 Ba 430 75 873 1907 Th 26.44 13.45 24.67 10.55 Nb 43.99 24.56 43.17 9.15 Y 47.19 20.50 56.26 17.71 Hf 6.35 3.90 9.86 7.11 Ta 3.31 1.76 3.15 0.73 U 6.20 3.26 5.79 3.42 Pb 27.01 13.89 28.02 15.12 Rb 168.7 108.2 169.2 99.1 Cs 4.09 1.88 4.01 2.21 Sr 22 5 52 438.71 Sc 2.9 1.1 5.5 13.88 Zr 176.0 110.8 356.9 282.4 206Pb/204Pb 17.69 17.62 17.87 21.91 207Pb/204Pb 15.61 15.60 15.66 16.51 208Pb/204Pb 38.37 38.34 38.52 40.52 87Sr/86Srm 0.70993 0.71019 0.71954 0.72873 2 σ error 0.00007 0.00007 0.00007 0.00004 143Nd/144Nd 0.512253 0.512253 0.512151 0.510803 2 σ error 0.000023 0.000023 0.000023 0.000012 epsilon Nd -7.5 -7.5 -9.5 -35.8 * picked glass was analyzed using 8mm beads, approximately 1 g of powdered sample **picked glass from samples supplied by Kathryn Watts and Dr. Iilya Bindeman, sample YC96-2G from Bindeman and Valley (2001) TSC - Tuff of Sulphur Creek, CAN - Canyon flow, DRF - Dunraven Road flow, BBF - Biscuit Basin Flow (south, north, east)

87Sr/86Sr ratios of separated plagioclase phenocrysts were measured using a New Wave UP-213 laser ablation system and analyzed using a Thermo-Finnigan Neptune multi-collector ICP-MS (LA-MC-

ICP-MS) in the GeoAnalytical Laboratory at Washington State University (data presented in Online

Resource). Ratios for each sample were collected 100 times and averaged, then corrected for mass bias and interferences. An in house plagioclase standard, IBS was used for corrections. See Ramos et al.

(2004) for further discussion of the method and http://www.wsu.edu/~geolab for additional instrument information.

Table 10. Average feldspar chemistry from the EUBM

Tuff of Sulphur Tuff of Sulphur Unit Canyon flow Dunraven Road flow Canyon flow Creek Creek mineral plagioclase plagioclase plagioclase alkali feldspar alkali feldspar (wt%) n = 57 2 σ n = 29 2 σ n = 23 2 σ n = 113 2 σ n = 8 2 σ

SiO2 61.94 2.43 61.95 3.00 61.28 1.29 64.73 1.15 64.80 0.78

Al2O3 23.53 1.74 24.00 2.21 23.15 0.67 19.73 0.54 19.95 0.26 FeO 0.32 0.06 0.31 0.04 0.32 0.05 0.20 0.05 0.20 0.05 CaO 5.02 1.88 5.28 2.28 4.88 0.62 0.76 0.30 0.82 0.15

Na2O 7.49 0.65 7.56 0.79 8.69 0.38 5.16 0.48 5.29 0.21

K2O 1.57 0.81 1.39 0.68 1.15 0.38 7.97 0.84 7.80 0.37 BaO 0.22 0.14 0.22 0.13 0.18 0.11 1.60 0.69 1.72 0.22 Total 100.10 0.99 100.70 0.62 99.66 0.88 100.15 0.95 100.58 0.69

An 24.55 9.12 25.60 10.85 22.22 2.90 3.87 1.52 4.16 0.72 Ab 66.33 5.38 66.39 7.14 71.55 2.80 47.68 3.78 48.63 1.78 Or 9.12 4.71 8.01 3.93 6.23 2.03 48.45 5.13 47.21 2.20 (ppm) n = 5 n = 6 n = 7 n = 9 n = 2 Rb 5.36 5.41 3.35 3.83 3.49 2.38 124 101 51.6 0.16 Sr 434 78.1 355 305 191 24.9 251 183 408 74.3 Y 0.98 2.21 0.80 0.68 0.34 0.41 2.58 4.41 5.90 4.80 Cs 0.03 0.07 0.00 0.00 0.01 0.06 0.18 0.17 0.10 0.18 Ba 1370 806 1330 1350 976 254 7840 5390 10340 63 La 20.5 12.2 18.6 17.1 14.5 2.86 12.2 8.26 14.5 6.76 Ce 30.4 14.8 25.6 22.1 21.7 3.45 14.1 14.26 14.1 5.40 Pr 2.08 0.99 1.79 1.51 1.37 0.27 1.03 1.20 0.93 1.08 N 6.37 4.79 5.05 4.20 3.62 0.77 3.34 4.43 3.00 4.67 Sm 0.70 0.64 0.49 0.44 0.35 0.08 0.58 1.17 0.47 0.86 Eu 6.40 1.43 5.26 4.65 2.33 0.23 4.72 2.46 7.43 0.16 Gd 0.52 0.52 0.76 0.70 0.24 0.08 0.64 0.90 5.41 1.35 Tb 0.04 0.07 0.03 0.04 0.02 0.02 0.07 0.14 0.06 0.12 Pb 20.0 5.35 17.8 15.8 19.3 2.28 38.0 18.0 29.7 0.58

Results

Physical Description of the EUBM rhyolites:

The EUBM is approximately 481 ± 8 ka (Gansecki et al., 1996) and has been described as including four units: Tuff of Uncle Tom’s Trail, Tuff of Sulphur Creek, Canyon flow, and the Dunraven

Road flow, from oldest to youngest. The Tuff of Uncle Tom’s Trail is located between Upper and Lower

Falls in the Canyon area of Yellowstone and is at least 35 m thick over an approximately 2 km2 area

(Christiansen, 1999; Christiansen 2001). Outcrops are generally well bedded, poorly sorted, and contain layers of dense pumice and lithics ranging from Eocene Absaroka volcanics to obsidian fragments.

Christiansen (2001) describes this unit as a pyroclastic flow deposit overlain by a diamicton. The Tuff of

Uncle Tom’s trail was most likely mapped separately from the Tuff of Sulphur Creek based on depositional styles, as the Tuff of Sulphur Creek has been described as an agglutinated air fall tuff

(Christiansen and Blank, 1972).

The Tuff of Sulphur Creek is approximately 230 m thick and spans an elongated area of approximately 119 km2 making up the wall of the Canyon and extending many kilometers to the east.

The Tuff in the walls of the Canyon is densely welded and massive with faint columnar jointing and very faint lenses of increased phenocryst concentrations. The type location is north of Sulphur Creek where the unit grades, vertically and laterally, into a bedded deposit just outside of the caldera (Christiansen and

Blank, 1972). Approximately 230 m to the east along the same cliff where Christiansen and Blank (1972) described this unit there is a complete basal section of the Tuff of Sulphur Creek. At this outcrop, there are two matrix-supported layers (each approximately 2 m thick) made up of poorly sorted ash, pumice and blocks overlying Eocene Absaroka volcanics. Welding increases from the base to the top of each layer. However, both layers are still moderately welded and do not allow for sieving of undisturbed samples (Figure 21). Many of the pyroclastic features, such as fiamme, rounded and fragmented pumices

(imbricated at the upper portion of the bottom layer), poorly sorted glass fragments, and lithics are

preserved. Separating these two layers is a thin, approximately 1 cm, layer of sand to fine gravel sized clast-supported black obsidian fragments and welded pumices. These black obsidian fragments have a distinct chemical composition of a more evolved high silica rhyolite and can be found in trace abundances throughout the basal layers. Similar black obsidian fragments are found in the Tuff of Uncle Tom’s Trail.

Overlying the basal layers is a vitrophyre which displays increased welding towards the top of the 2 to 3 m thick layer. Pyroclastic features are present in thin sections from the base, but are absent in samples from the top because welding has obscured most features. Overlying the basal vitrophyre is a thick section of devitrified tuff containing fiamme ranging from 1 mm to 10 cm long. Outside of the caldera the Tuff of Sulphur Creek is comprised of thinly bedded devitrified layers with variable vesicle and lithic content. Some of the thin (approx 0.25 m thick) layers contain angular glass fragments up to 5 cm in length within an ashy groundmass that show similar chemical composition to the rest of the unit.

Figure 21. Generalized cross section of the eastern Upper Basin Member rhyolites.

Field observations and thin section analyses indicate that the Tuff of Sulphur Creek is most likely a pyroclastic flow deposit. The type location, initially described as an agglutinated ash-fall tuff located outside of the ring fracture, is better described as a veneer deposit where the pyroclastic flow encountered a topographic high and the upper, more dilute portions of the current overtopped topography created by ring fracture blocks. Such lateral variability lithofacies are common features of pyroclastic density current deposits (Branney and Kokelaar, 2002). The Tuff of Sulphur Creek, therefore, most likely correlates with the Tuff of Uncle Tom’s Trail.

The next highest unit in the EUBM is the Canyon flow. This unit covers the Tuff of Sulphur

Creek over an area of 118 m2 and is approximately 20 m thick. The Canyon flow is only discernable from the Tuff of Sulphur Creek where flow banding is present. Outcrops are generally found in depressions within the Tuff of Sulphur Creek and appear to fill topographic lows. Outcrops consist of a basal vitrophyre which can be up to 4 m thick, but is commonly on the order of 1 m thick. Thick basal vitrophyre can contain spherulites up to 5 cm in diameter, but spherulites are generally minor where the basal vitrophyre is thinner. The stony interior is generally a light gray devitrified rock with light red to pink bands and can be up to 20 m thick in some areas. The glassy upper portion of the Canyon flow is 2 m thick and in multiple locations is a highly vesiculated breccia. At the eastern end of the Canyon flow the upper portions also contain a thin layer of volcanic sediments. Distinguishing between possible multiple flows is difficult due to sparse exposures. However, Pb and Nd isotope ratios measured on a sample from just west of Silver Cord Falls suggest that there may be more than one flow in this unit.

Sample 0822 from Silver Cord Falls contained 206Pb/204Pb = 17.54, 207Pb/204Pb = 15.59, 208Pb/204Pb =

38.23, which are lower than other whole rock Pb isotope measurements from the Canyon flow, which are generally around 17.81, 15.65, and 38.37, respectively. This may indicate that the area near Silver Falls contains a younger flow as the sample appeared to be taken from the brecciated upper part of the unit, along the top of the Canyon rim. Similar sequences also appear in the WBUM, where older units contain more radiogenic isotopic ratios than younger flows.

The Dunraven Road flow overlies the Canyon flow in the northeastern portion of the caldera. The

Dunraven Road flow has been described by Christiansen (2001) as having a vitric basal breccia and extending to the Canyon rim, covering an area of 4 km2. Further mapping and chemical analysis have found that the Dunraven Road flow is only approximately a quarter of the originally mapped size (1.2 km2) and resembles a rhyolitic dome centered on the northeastern portion of the ring fracture (Figure 22).

The previously mapped basal breccia contains up to 20% phenocrysts and is chemically similar to the upper breccia of the Canyon flow.

Figure 22. Map of the Dunraven Road flow (Qpud). The original boundary is presented in light shade (Prostka et al, 1975;

Christiansen, 1999) and boundary from this study presented with a dark outline.

Mapping has also revealed that the Dunraven Road flow sample analyzed by Bindeman and

Valley (2001) was most likely taken from the Canyon flow, which explains discrepancies between stable isotope ratios measured by Bindeman and Valley (2001) and Hildreth et al. (1984). The central portion of the Dunraven Road flow is exposed within a valley mapped as the ring fracture/caldera boundary by

Prostka et al. (1975). The core of this high silica rhyolite is approximately 20 m thick. The core is

devitrified and heavily flow banded, almost swirly, in parts. Surrounding the core is a layer of vitrophyre that can be up to approximately 10 m thick and at the extremities of the unit is heavily spherulitic, such as is found in multiple road-cuts along Dunraven Pass Road. Closer to the core of the unit, however, the glass lacks spherulites and can contain black and red banded obsidian.

Whole Rock Geochemistry

EUBM whole rock geochemistry and glass geochemistry are presented in Hildreth et al. (1991) and Girard and Stix (2009). However, for this study samples were collected throughout and across the units, and describe greater heterogeneity than described in previous work. A summary of whole rock and glass data are presented in Tables 2 and 3.

Analyses of the Tuff of Uncle Tom’s Trail were completed using microprobe and LA-ICP-MS on pumices as well as XRF and ICP-MS on large angular glass inclusions. Many of the samples have been hydrated and hydrothermally altered. Therefore, correlation between the Tuff of Uncle Tom’s Trail and the Tuff of Sulphur Creek based on geochemistry alone is not definitive, but due to both tuffs having mapped correlations in the field and generally similar chemistries we propose that the two are indeed the same unit, with Tuff of Uncle Tom’s Trail representing the western-most extent of a larger ignimbrite.

The Tuff of Sulphur Creek and Canyon flow are high silica rhyolites and show relatively high concentrations of FeO, TiO2, Sr, Ba, and Sc when compared to other Yellowstone rhyolites, which may indicate less fractional crystallization and/or a more fertile source. Melt inclusion data presented by

Gansecki (1998) were approximately 1.2 percent water and very similar glass compositions for the

Canyon flow. Differences between the major elements are within error, although the melt inclusions generally have lower SiO2 and higher Al2O3.

Dunraven Road flow has higher SiO2 concentrations, but generally plots with other rhyolites from

Yellowstone for most elements and does not show increased FeO, TiO2, Sr, Ba, and Sc as found in the

Tuff of Sulphur Creek and Canyon flow. Rare earth elements analyzed from the EUBM also indicates

that Dunraven Road flow has depleted values compared to Tuff of Sulphur Creek and Canyon flow

(Figure 23).

Figure 23. Rare Earth Element plot for whole rock samples from the EUBM. Values are normalized to Bulk Silicate Earth

(McDonough and Sun, 1995). Figure 8 is a similar diagram with results from the Silver Cord flow as well.

Mineralogy/Petrology

The mineral assemblages of the Tuff of Uncle Tom’s Trail, Tuff of Sulphur Creek, and Canyon flow are very similar. Tuff of Uncle Tom’s Trail contains small (5 mm) obsidian fragments, auto- brecciated glass, and porphyric sections of groundmass appear to be very similar to the basal sections of

Tuff of Sulphur Creek. As found in this study and Girard and Stix (2009), the mineralogy of the

Dunraven Road flow is very different from the other EUBM.

Tuff of Sulphur Creek contains phenocrysts in variable concentrations, from approximately 10 to

20 percent in the basal sections with 20 to 35 percent in the stony interior. Plagioclase phenocrysts make up approximately 5 to 15 percent of samples and range from An18 to An37, with an average of An25 (Table

3). Cores of larger, sometimes sieved, plagioclases are generally more calcic, An24 to 30, similar to observations by Girard and Stix (2009). Magma compositional changes are also indicated by a small proportion of the larger plagioclase laths having coronas with compositions of alkali feldspar. Anti- rapakivi texture is also observed in samples from Canyon flow and Huckleberry Ridge Tuff C, which may indicate that either cooler temperatures or mixing with silicic magma occurred just prior to eruption

(Figure 24). Alkali feldspar phenocrysts make up approximately 5 to 20% of the samples and range from

Or40 to Or55, with an average of Or48. Alkali feldspars from Tuff of Sulphur Creek, Canyon flow, and

HRT-member C contain high amounts of Ba, generally over 1 weight percent, which is a greater concentration than found for other units at Yellowstone (Gansecki, 1998). Quartz phenocrysts make up 5 to 15 percent and are commonly fragmented and occasionally embayed. Oxides, mostly ilmenite and titanomagnetite, are also present in variable abundances, about 2 to 5 percent. Oxides tend to have rather high Mn concentrations (approximately 1 weight percent). Traces of pyroxene and zircon are also present in samples from the Tuff of Sulphur Creek. One amphibole grain with a heavily oxidized rim was observed within the vitric base of the Tuff of Sulphur Creek. Amphibole is lacking in most thin sections and past published petrographic descriptions, but may have existed in the magma at higher pressures

(Rutherford, 2008). Fine grained lithic fragments are also present up to approximately 5 percent in the basal ash, vitrophyre, and some of the upper banded portions of the veneer deposit. Thin sections made from the basal poorly sorted ash and pumice further provide evidence for deposition by pyroclastic density current due to large variety in grain sizes and variably sized large bubble wall shards (Figure 25a, b).

Canyon flow phenocrysts are variable in concentration, but not to the same extent as in the Tuff of

Sulphur Creek. Phenocrysts generally make up 15 to 35 percent and feldspars are variable in composition. Plagioclase phenocrysts make up approximately 5 to 15 percent of samples and range from

An19 to An40 with an average of An25 (Table 10). Similar to Tuff of Sulphur Creek, cores of larger

plagioclase tend to have a slightly higher anorthite component at An24 to An40, when compared to rims of

An19 to An27. Plagioclase textures are similar to those in the Tuff of Sulphur Creek, including sieved cores, resorbed rims, and occasional anti-rapakivi (Figure 24). Alkali feldspar phenocrysts make up approximately 5 to 25 percent of the samples and range from Or40 to Or54, with an average of Or48.

Quartz phenocrysts make up 5 to 15 percent of the samples and are commonly embayed.

Figure 24. a) Backscatter image of anti-rapakivi texture from the Canyon flow, sample 08CP21B. b) Distance from rim versus percent anorthite (An), albite (Ab), and orthoclase/sanidine (Or) from results from electron microprobe transect from the rim to core-region. Titanomagnetite core, nine points from the alkali feldspar rim and plagioclase core shown in the graph. Extent of crystal is outlined with a thin black line.

Figure 25. a) and b) 50 times magnification photomicrographs from the base of Tuff of Sulphur Creek, sample 08CP29, showing poorly sorted bubble wall shards and ash. c) 50 times magnification image of Dunraven Road flow, slide 08CP01, showing ribbon like features that may be oxidized microfractures. Crystallites are also present as isolated features and clumped into masses, as depicted in the lower left hand corner. d) 200 times magnification image of crystallites from the same slide as (c). e) a backscatter image of microfractures, showing lighter colors around the edges of fractures.

Pyroxenes are trace components in the stony interior of the Canyon flow. Up to 6 percent is found in the basal vitrophyre; it is commonly associated with plagioclase and oxides in aggregates. In basal samples, approximately 4 percent are augite, Wo39-40En31-35Fs25-29, (similar to data presented by

Hildreth et al., 1991; Girard and Stix, 2009) and 2 percent are ferrosilite, Wo3-4En41-43Fs53-55. Ferrosilite was found exclusively in aggregates, whereas the augite was found in aggregates and as isolated crystals.

Pyroxenes contain more Mg than others measured from the caldera (Hildreth et al., 1984). Other phenocrysts included oxides and trace zircon. Quartz rich lithic fragments were prevalent in the basal vitrophyre, but were not found in the stony interior.

The Dunraven Road flow is very distinct from the other EUBM units in that it is aphanitic with up to 8 percent plagioclase phenocrysts. Phenocryst compositions are very different to those in the Tuff of Sulphur Creek, ranging from An19 to An24, with an average of An22 and no discernable difference from core to rim. Plagioclase phenocrysts also contain much less Sr, Ti, and Rb, and are generally lower in trace element concentrations when compared to the other EUBM rhyolites (Table 10). Oxides can range up to about 5 percent and are generally titanomagnetite, with much less Mn than the other EUBM rhyolites. Quartz and sanidine may be found as trace minerals, but are often very small. Black and red obsidian samples from the Dunraven Road flow commonly contain features that resemble small red ribbons throughout thin sections (Figure 25c). We have interpreted these features as microfractures due to the presence of occasional conchoidal fracturing with the ribbons. Backscatter images of the ribbons

(Figure 25e) show that the edges of the ribbons can have slightly higher FeO concentrations. The slight increase in FeO is interpreted as precipitated and oxidized iron. Based on the alignment of the microfractures, these features appear to have formed during cooling. Oxidation may have occurred during cooling or as part of the weathering process. Crystallites are also present as small cross shaped splinters on the order of 100 nm, and tend to accumulate in bands and blobs. The presence of crystallites

(microscopic crystal nucleations) may indicate that the magma was too viscous to allow crystal growth

(Figure 25d) (Best, 2003).

Temperature and Viscosity

Magmatic temperatures of the EUBM were estimated with applicable geothermometers. Using plagioclase-melt calculator by Putirka (2008) the Tuff of Sulphur Creek and Canyon flow were

o approximately 890 and 887 C, respectively. Calculations used variable concentrations of H2O (1.8 to 3 percent) based upon values found by Gansecki (1998) and common values of rhyolite. Temperatures ranged from 857 to 825oC for the Dunraven Road flow. The temperature of the Dunraven Road flow is most likely lower than other EUBM rhyolites by approximately 33 to 65 oC. Ternary feldspar thermometry (Putirka, 2008) was used on rims of plagioclase and alkali feldspars from the Tuff of

Sulphur Creek and Canyon flow and yielded temperatures of 868oC and 866oC, respectively. Using pyroxene-melt geothermometers (Putirka, 2008) the Canyon flow temperature was calculated to be approximately 860oC. However, previous studies have measured temperatures using oxide-oxide geothermometry for the Tuff of Sulphur Creek and Canyon flow from 850 to over 900oC (Hildreth et al.,

1984; Bindeman and Valley, 2001). The temperature for the Tuff of Sulphur Creek is, therefore, at least

850oC and the Dunraven Road flow is estimated to be approximately 816oC. Based on these temperatures and average whole rock chemistry the viscosity for each flow has been estimated at 8 x 106 Pas for Tuff of Sulphur Creek, 4 x 106 Pas for Canyon flow, and 2 x 107 Pa sec for Dunraven Road flow (Giordano et al., 2008).

Radiogenic Isotope Ratios

Radiogenic isotope data are presented in Table 2 and Figures 26 and 27. Most of the Upper Basin

Member rhyolites have more radiogenic 87Sr/86Sr, 206Pb/204Pb, and 207Pb/204Pb ratios than other

Yellowstone rhyolites (Doe et al., 1882; Hildreth et al., 1991). Huckleberry Ridge Tuff, member C

(HRT-C) contains more radiogenic 87Sr/86Sr, 206Pb/204Pb, 207Pb/204Pb, and lower 144Nd/143Nd ratios when compared to other Yellowstone volcanics, including the EUBM. The Blue Creek flow and Mt. Jackson

rhyolites, which are post-HRT-collapse rhyolites show similar trends to the UBM rhyolites, with depleted

δ18O values and somewhat enriched 87Sr/86Sr values (Hildreth et al., 1991).

Sample 0822, taken from the devitrified upper portion of the Canyon flow, located near Silver

Cord Falls, contains 206Pb/204Pb, 207Pb/204Pb , 208Pb/204Pb and 144Nd/143Nd values that are similar to other intracaldera rhyolites, and much less radiogenic than other samples from the Canyon flow (Table 9).

Variations in radiogenic isotope ratios may suggest that there are multiple flows in the Canyon flow. The name Silver Cord Falls flow is here referred to this youngest flow of the Canyon flow.

The Dunraven Road flow contains very similar ratios of 87Sr/86Sr, 206Pb/204Pb, 207Pb/204Pb,

144Nd/143Nd when compared to extra-caldera rhyolites, most notably the Roaring Mountain Member. The

Dunraven Road flow also contains low 208Pb/204Pb ratios when compared to other Yellowstone rhyolites

(Figure 28), indicating that the source rock may have had very low Th. Three Dunraven Road flow samples were run at different times to validate the results, and all the data for the Dunraven Road flow

(except δ18O ratios) are relatively homogeneous. The Scaup Lake flow is plotted from data published by

Vazquez et al. (2009) for sample YCV08, with an unpublished 87Sr/86Sr value of 0.709838 ±11, measured by TIMS (Vazquez, personal communication).

87Sr/86Sr was measured on picked plagioclase phenocrysts from the Tuff of Sulphur Creek,

Canyon flow, and Dunraven Road flow (Figure 28). Some grains are in equilibrium with the melt, whereas most have more radiogenic values. There does not seem to be any correlation between core, rim, or size of the phenocryst, although samples were fractured (chipped) prior to picking. Thus, small plagioclase phenocrysts may have been fractured portions of larger grains. Data may be interpreted as evidence that the rhyolites are rejuvenated crystal mush (Girard and Stix, 2009), but that the pre-existing magma had more radiogenic values than the replenishing magma, which may be the case if assimilation of Archean crust influenced rhyolite genesis.

87 86 147 144 Figure 26. Sr/ Sr (480ka) and Nd/ Nd plot of rhyolitic groups from Yellowstone. Eocene volcanics (Feeley et al., 2002), and

Beartooth Mountains (Wooden and Mueller, 1988) plotted for comparison. Basalts from within the Yellowstone Plateau area,

HRT – Huckleberry Ridge Tuff (members A, B, & C), LCT – Lava Creek Tuff (members A & B), BBF – Biscuit Basin flows

(denoted by N-north, S-south, M-middle, and E-east), bc- Blue Creek flow, mj – Mt. Jackson rhyolites. Dunraven Road flow plots within the extra-caldera zone. Data for Yellowstone Samples from: Doe et al., 1982; Hildreth et al., 1991; Bennet, 2002;

Nastanski, 2002; Vazquez et al., 2009; and this study. Models A thru D are EC-RAxFC curves, discussed in text.

Figure 27. Measured 208Pb/204Pb and 207Pb/204Pb versus 206Pb/204Pb plot of rhyolitic groups from Yellowstone. Basalts from within the Yellowstone Plateau area, HRT – Huckleberry Ridge Tuff (members A, B, & C), LCT – Lava Creek Tuff (members A

& B), BBF – Biscuit Basin flows (denoted by N-north, S-south, M-middle, and E-east). Data for Yellowstone Samples from:

Doe et al., 1982; Hildreth et al., 1991; Bennet, 2002; Nastanski, 2002; Vazquez et al., 2009; and this study. Beartooth Mountain samples are highly variable and span the entire plot area, and more.

Figure 28. Results from laser 87Sr/86Sr for plagioclase picked from the Tuff of Sulphur Creek, Dunraven Road flow, and Canyon flow. Maximum and minimum 87Sr/86Sr values of glass and whole rock for each unit are depicted for comparison.

Stable Isotope Ratios

The EUBM and WUBM rhyolites have been shown to be low-δ18O rhyolites by multiple studies

(Friedman, 1976; Hildreth et al., 1984; Bindeman and Valley, 2001; Bindeman et al., 2008). Our measurements of stable isotope ratios for the Tuff of Sulphur Creek and the Canyon flow generally agree with previously measured quartz and feldspar ratios, although they are occasionally higher than those of

Hildreth et al. (1984), Bindeman and Valley (2001), and Bindeman et al. (2008). Quartz from the base of the Tuff of Sulphur Creek (picked from pumices) and from the vitric base of the Canyon flow consistently have higher δ18O values (2.4‰, n=4) than the rest of the unit which averaged 1.8‰ (n = 10). Quartz picked from the base of Canyon flow also exhibited higher δ18O values (3.0‰, n= 2) when compared to the rest of the unit which averaged 2.5‰ (n=4). Not including the basal portions of each flow and assuming a magma temperature of 850oC, the Tuff of Sulphur Creek magma was approximately 1.2‰ and the Canyon flow magma was approximately 1.8‰ (Zhao and Zheng, 2003).

δ18O values for plagioclase separates from the Dunraven Road flow ranged from 2.6 to 4.8‰

(n=9). These values are comparable to those found by Hildreth et al. (1984). Sample YL96-4 from

Bindeman and Valley (2001) was most likely from the Canyon flow, based on the location and description of the sample, though published as a sample from the Dunraven Road flow. We also analyzed quartz grains from the devitrified core of the Dunraven Road flow. Quartz values from the Dunraven

Road flow were significantly lower than the plagioclase feldspar (1.5‰); however, quartz present in the devitrified section of Dunraven Road flow is most likely vapor phase. Quartz was only observed in elongated vesicles and not in the vitric portions of the flow. The average plagioclase phenocryst δ18O value for the Dunraven Road flow was 4.0‰. Assuming a magmatic temperature of 800oC, the magmatic value of the Dunraven Road flow is approximately 5‰, with an error of approximately 1‰ due to high variability in the plagioclase phenocrysts (Zhao and Zheng, 2003). This value agrees well with δ18O values measured from obsidian (Hildreth et al., 1984).

Studies of quartz and zircon δ18O values by Bindeman et al. (2001 to 2008) found that minerals from rhyolites that immediately followed caldera collapse have normal δ18O cores with low-δ18O rims, whereas the younger Central Plateau Member and Scaup Lake flow contain low-δ18O cores with normal

δ18O rims (Bindeman et al. 2008). Such observations suggest that older units had a source rock that was initially not depleted in δ18O, whereas younger units had a source that was depleted in δ18O ratios and shifted to more normal values (Bindeman et al., 2008). Bindeman et al. (2008) also found that HRT members B and C, Lava Creek Tuff, and Mesa Falls Tuff also exhibit some degree of depleted δ18O values, whereas HRT member A contains somewhat higher δ18O values. We analyzed grains from a sample of the Archean basement and found that quartz, plagioclase, alkali feldspar, and biotite are: 8.7‰,

7.0‰, 7.0‰, and 3.8‰, respectively. If values from the Archean basement reflect the source values then depletions found in the EUBM may be as high as 5.8‰, assuming an original magmatic δ18O value of

7.0‰ as reflected by the value of Archean alkali feldspar.

Discussion

Rhyolite genesis is generally thought to involve partial melting of the crust (Doe et al., 1982;

Hildreth et al., 1991; and Christiansen, 2001). However, multiple processes for rhyolite genesis have been presented in the literature, where the only similar factor is that the rhyolites have generally undergone fractional crystallization prior to eruption. We would like to address the plausible processes that can lead to the genesis to the EUBM, and to lesser extent rhyolites from the Yellowstone volcanic area in general. As illustrated by Hildreth and other (1991) and emphasized in this paper, deciphering the genesis of these rhyolites is complex and given the diversity of the crust the concept of making simple mixing curves is fairly futile. However, integrating data from physical volcanology, petrology, geochemistry, and geophysics allow a conceptual model for understanding genesis of the Yellowstone rhyolites. Any model requires the consideration of the following observations:

1) Isotopic shifts are found following the large scale caldera collapses at 2.1 Ma and 640 ka

(Hildreth et al., 1991), slight δ18O depletions have also been found in HRT members B and C,

Lava Creek Tuff, Mesa Falls Tuff, and the rhyolites of the Central Plateau Member (Hildreth et

al., 1984; Bindeman et al., 2008)

2) Low velocity zones from seismic tomography depict the top of crystallizing magma body at

depths of 8 km (Husen et al., 2004) and possibly basaltic sills at a depth of 15 km (Wicks et al.,

2006).

3) Plagioclase phenocrysts have oligoclase to andesine cores with oligoclase rims (Girard and Stix,

2009) and most grains (independent of core or rim location) contain more radiogenic 87Sr/86Sr

ratios than the host magma.

4) Zircon ages do not generally exceed 2.5 Ma and no Archean age zircons have been found in

Yellowstone rhyolites. Zircons from caldera forming eruptions indicate that crystallization

occurred over the span of 10’s to 100’s of thousands of years (Bindeman et al., 2008).

5) Quartz and zircons from Canyon flow contain cores with higher δ18O values than the rims

(Bindeman et al., 2008). The base of the Tuff of Sulphur Creek and Canyon flow contain

phenocrysts with higher δ18O values than the rest of the flow. The base of the Tuff of Sulphur

Creek also contains up to 20% fewer phenocrysts than the stony interior.

It has been suggested that Yellowstone rhyolites may be formed by: 1) Partial melting of Earth’s crust (Doe et al., 1982; Hildreth et al., 1991; Christiansen, 2001), 2) Melting of previous volcanic deposits from the Yellowstone volcanic area (Bindeman and Valley, 2001), 3) Partial melting of hydrothermally altered un-erupted magma and volcanic deposits with a rejuvenation of crystal mushes (Girard and Stix,

2009), and 4) In this paper we model the EUBM rhyolites using the Energy-Constrained Recharge,

Assimilation, and Fractional Crystallization model (EC-RAxFC), as developed by Spera and Bohrson

(2002) and Bohrson and Spera (2007). The following is a brief description of these plausible mechanisms for rhyolite genesis.

Partial melting of the crust is the generally accepted method to form voluminous rhyolites and explain the absence of intermediate volcanic rocks at Yellowstone. We have used batch melting equations to produce a model where an approximately 30% partial melt can produce the rare-earth element values found in Yellowstone rhyolites, including the Tuff of Sulphur Creek and Canyon flow. If the magma chamber started with a typical Yellowstone radiogenic signature (for example: Lava Creek

Tuff, member A) the more radiogenic signature of the EUBM can be achieved by assimilation of 15 to

25% of more radiogenic crustal material (Hildreth et al., 1991). To form low-δ18O rhyolites requires the crustal assimilant to be approximately -12‰.

On the scale of a crystal, more calcic cores from plagioclase phenocrysts for the Tuff of Sulphur

Creek and Canyon flow have been described “as retained residual feldspars from partial melting of the crust” (Doe et al, 1982). To test this hypothesis, plagioclase crystals from Archean crust at Lamar

Canyon were measured. Analyzed Archean plagioclase compositions were An19-30, Ab69-81, and Or1. If

plagioclase phenocrysts were inherited from Archean gneiss this would require significant exsolution of the grains, or recrystallization to increase Or percent, and decrease the Ab component prior to eruption of the EUBM. Although occasional perthitic textures are observed, extensive exsolution lamellae are not preserved in most phenocrysts from the EUBM (Hildreth, et al., 1984), though such features could be immersion in magma. Laser 87Sr/86Sr measurements of plagioclase phenocrysts are generally more radiogenic than the surrounding glass, but require that 87Sr/86Sr values of the crustal material were approximately 0.717 to 0.718. This is significantly less than our measured value of Archean granitic- gneiss from Lamar Canyon (0.72873 ± 4) and significantly less than estimated values of Hildreth et al.

(1991), but within the measurements of the Beartooth Mountains (Figure 26) (Meen, 1987). However, since Sr is generally more compatible into feldspars, lower Rb/Sr ratios would be expected in the feldspars, leading to less radiogenic values. So we are not certain what percentage of phenocrysts were inherited from the Archean, if at all.

Melting of hydrothermally altered volcanic rocks from previous eruptions of Yellowstone rhyolites has been suggested as the source for UBM rhyolites, and other volcanic centers along the eastern

Snake River – Yellowstone Hotspot Track (Bindeman and Valley, 2001; Bindeman et al., 2007;

Bindeman et al., 2008). UBM radiogenic values are then explained in this model by inheritance from previously erupted Yellowstone rhyolites (Bindeman et al., 2008). The only other Yellowstone volcanic rock to have such an anomalous radiogenic isotope composition is HRT-C. HRT-C also has similarities to the UBM rhyolites, such as high Ba concentrations in alkali feldspar, and anti-rapakivi texture samples.

However, HRT-C only has an estimated volume of 250 km3 (Christiansen, 2001). The approximate volume of Tuff of Sulphur Creek and Canyon flow is a little over 100 km3. Based on volumes of HRT-C and EUBM, over half of the deposition of HRT-C would have been deposited 60 km to the northeast, where no HRT-C has been mapped outside, or within the caldera. Furthermore, more radiogenic values preserved in phenocrysts suggests that the source rock contained higher radiogenic values than older

volcanic events at Yellowstone, except for HRT member C, making inheritance of radiogenic isotopes difficult to form the eastern Upper Basin Member.

We have attempted to apply EC-RAxFC (Bohrson and Spera, 2007) as presented in Figure 26.

We prefer EC-RAFC because:

1) 87Sr/86Sr and 143Nd/144Nd for EUBM rhyolites and HRT-C can be modeled with measured data,

whereas simple mixing of crust with mantle derived material requires unrealistically low Nd

and/or high Sr concentrations in end members.

2) Plagioclase phenocrysts contain higher 87Sr/86Sr ratios than glass and whole rock, suggesting a

mix of a more and less radiogenic source material.

3) There is an ample heat source, basalt injections, to allow for recharge of magma chambers and

allow for assimilation with less crystallization than described by Glazner (2007).

4) Disaggregation of xenoliths explains why few xenoliths are found and zircon ages do not extend

to the Archean (Beard et al., 2005).

5) Assimilation of crust by multiple magma chambers allows for large amounts of rhyolite to be

formed without exorbitant uplift rates, and emplacement rates on the order of 100’s of thousands

of years can be achieved by “incremental assembly” (Coleman et al., 2004).

6) Upper Basin Member rhyolites tend to plot on similar model curves with low equilibration

temperatures/high amounts of assimilation and may signify magma that interacted with cool wall

rock and underwent high amounts of fractional crystallization and was therefore unable to erupt.

7) Similar problems with creating 87Sr/86Sr and 143Nd/144Nd values for rhyolites in the Eastern Snake

River Plain have been explained by using EC-AFC (McCurry et al., 2008), although intermediate

rocks are present in that system.

EC-RAxFC models can be made for all of the Yellowstone rhyolites using measured data and variable equilibration temperatures. UBM protoliths are formed with relatively high amounts of assimilation and fractional crystallization, resulting in lower equilibration temperatures. Four models are shown in Figure 26. Models A and B are based on a mixture of Junction Butte basalt (Hildreth et al.,

1984) and Archean Basement (Lamar Canyon – sample 08CP61), with recharging magma that is similar to Junction Butte basalt. Models C and D replaced Junction Butte basalt with Swan Lake basalt values, as the rocks being modeled were extra-caldera rhyolites, although models using either basalt yielded similar results. Variables used in the models include: initial basaltic temperature of 1184oC, calculated using

MELTS (Ghiorso and Sack, 1995), initial wall rock temperature of 450oC (using lower wall rock temperatures for Model A, did not substantially change the model), and a resulting magma solidus of

750oC (estimated from MELTS and assumed to be lower than the magmatic temperatures for EUBM).

Model curves are presented in Figure 26, where Models A and B, and C and D use the initial variables as described above with the exception of equilibration temperatures (Teq)/ Mass of assimilated wall rock

o o (Mao). Teq / Mao values for each model are: Model A 894.03 C / 2.091, Model B 910.05 C / 1.848, Model

C Junction Butte basalt 933.37oC / 1.496 (Swan Lake basalt: 915.88oC / 1.759), and Model D 1025.17oC /

0.970.

Variations in Teq are reasonable as the magmatic system below Yellowstone has been re- established after two large caldera collapses (2.1 Ma and 640 ka) and the wall rock temperature has most likely increased as the magma system has grown over time. Models A to D have increasing values of Teq to represent the influence of a slightly warmer wall rock with time. We propose that Model A represents the voluminous initial intrusions into cool wall rock. Model B is a homogenized magma chamber that feeds a bulk of Yellowstone rhyolitic volcanism. Models C and D (erupted units north of the caldera) appear to reach equilibrium at higher temperatures. Magma ascent seems to follow extensional structures north of the caldera and may require less interactions with the wall rock to rise through the upper crust and is generally considered the product of small and isolated magma chambers (Hildreth et al, 1991).

EC-RAxFC models fit the measured data. Variables for the model were based on measured data, whereas basic mixing requires un-realistic trace element concentrations for more radiogenic UBM and

HRT member C. Magma bodies in the Yellowstone caldera are initially made of smaller intrusions that have accumulated, or focused, in one area to produce a large rhyolitic magma chamber, as described for the Central Plateau Member rhyolites (Vazquez and Reid, 2002; Vazquez et al., 2009). Therefore, once a rhyolitic magma is established, by assimilation and fractional crystallization, the system contains a more radiogenic value than the intruding basalts; thus establishing two distinct radiogenetic magmas, as described by Christiansen (2001).

HRT-C is distinct from members A and B. It has been argued by Hildreth et al. (1991) that HRT-

C is in fact only a contaminated version of members A and B due to similar phenocryst assemblage and locality within the caldera of member A. Observations of anti-rapakivi texture may not be isolated to

HRT-C, although the presence of anti-rapakivi texture implies that a second recharge, or mixing event took place prior to eruption. HRT-C may have initially been at similar temperatures and pressures as of

HRT members A and B, however, even if the intrusive emplacement of HRT was similar for all members,

HRT-C may have erupted under different circumstances. For example HRT-C magma may have had higher levels of assimilation that were already too crystal rich to erupt, but was recharged or subsided during caldera collapse during the eruption of HRT members A and B. Bindeman et al. (2009) describe variable δ18O values in zircons from HRT members B and C, indicating that some digestion of hydrothermally altered material occurred prior to the eruption of the two younger HRT members, possibly indicating that assimilation of hydrothermally altered rock occurred just prior to eruption. Post HRT rhyolites, such as Blue Creek flow also show slightly increased radiogenic Sr ratios than common at

Yellowstone, with an associated depletion in δ18O values (Hildreth et al., 1991). Timing between the members of HRT is not known, but evidence suggests that HRT-C and Blue Creek may have formed similarly to EUBM rhyolites and that the HRT-C is more characteristic of a post-caldera rhyolite, although it is considered a caldera forming eruption.

Some EC-RAxFC factors that require consideration are that source rocks can vary greatly in trace element concentrations. Both the mafic and felsic end members have large variations in radiogenic Pb ratios. Christiansen (2001) described radiogenic lead coming from contamination by mixing with small amounts of basalt. However, in the case of radiogenic 206Pb/204Pb and 208Pb/204Pb ratios, both basaltic and wall rock values are extremely variable. For example, 206Pb/204Pb can vary from 15.02 to 36.36 in the

Beartooth Mountains (Wooden and Mueller, 1988; Meen 1987) and basalt 206Pb/204Pb ratios vary from

16.10 to 17.89. However, the more radiogenic isotope signature of the UBM requires a dominance of assimilated older bedrock.

Formation of low-δ18O rhyolites can be achieved by melting/assimilation of hydrothermally altered rocks (Taylor, 1980; Hildreth et al., 1991). To achieve the approximately -5.0 to -5.8‰ shifts found in post-caldera rhyolites, it has been proposed that meteoric water was the dominant fluid in hydrothermal alteration of source rocks; this also suggests very shallow melting (Bindeman and Valley,

2001; Bindeman et al., 2008). However, such shifts may also be influenced by time-integrated fluid flux during contact metamorphism over distances of approximately 10 km and at depth greater than a few kilometers (Dipple and Ferry, 1992). We propose that equilibration of δ18O during contact metamorphism may be a small portion of the hydrothermal alteration with meteoric water extending to depths along structural features. Meteoric water is the main fluid in hydrothermal systems at Yellowstone (Fournier,

1989; Larson et al., 2009). Modeling of caldera formation suggests that high angle normal faults are produced along the ring fracture with lower angle normal faults towards the center of the caldera, the approximate location of the resurgent domes, and may act as conduits for the establishment of deep hydrothermal circulation (Hardy, 2008). Therefore, meteoric water circulation and fluid-flux equilibration may be focused in areas such as the ring fracture and resurgent dome areas (Larson and

Taylor, 1986), which is where the UBM rhyolites are located.

Similar Sources for the Tuff of Sulphur Creek and Canyon flow

Similar whole rock chemistry, isotopic composition, phenocryst assemblage and composition, as well as juxtaposed position of the flows indicate that the Tuff of Sulphur Creek and Canyon flow are genetically similar. Pb isotopic ratios measured from a sample of Canyon flow taken from the Silver

Cord Falls area may indicate that there may be more than one flow mapped in the Canyon flow unit, and that this flow may show isotopic ratios comparable to the younger Central Plateau Member, North and

South BBFs, and Scaup Lake.

We prefer assimilation and fractional crystallization to explain the protolith for Tuff of Sulphur

Creek and Canyon flow as un-erupted magma, or intrusive rock. The intrusion may be as old as the

Huckleberry Ridge Tuff, 2.1 Ma, as this period of volcanism appears to have the largest amount of magma generated in the Yellowstone volcanic area and zircon grains have been dated to this time period

(Bindeman et al., 2008). These intrusions were more radiogenic than common Yellowstone rhyolites because of the high degree of assimilation. Cooled intrusions overlying the magma chamber were hydrothermally altered during a long history of underlying magmatic activity. The protolith was then dropped to melting depths during the last caldera collapse. We envision that the protolith was assimilated by any remaining magma, or slowly melted by latent heat from fractionated crystals. Phenocrysts from this protolith were then rejuvenated by the intrusion of rhyolite and erupted along the ring fracture/resurgent dome normal faults. Heterogeneity in these flows indicates that either the source rock was heterogeneous, or that mixing occurred prior to eruption as suggested by Girard and Stix (2009).

Figure 29 presents a generalized cartoon depicting the events leading to eruption of the EUBM rhyolites based upon EC-AXFC models A and C.

The close proximity of the Mt. Washburn volcanics suggests that Absaroka volcanics are a likely candidate as a source rock. Indeed, the Absaroka volcanics are described as forming by cryptic hybrid magmas, which involves the stalling of magma within the crust (Feeley et al., 2002). However, the distinct radiogenic signature of the Absarokas is very different than Yellowstone volcanics, with lower

87Sr/86Sr and much more radiogenic 144Nd/143Nd (Figure 26) and most likely did not contribute significantly to the intracaldera rhyolites.

Extra-Caldera Source for Dunraven Road flow

Petrology, geochemistry, and radiogenic isotope ratios suggest that the genesis of the Dunraven

Road flow is different from the rest of the EUBM. Small isolated volume, stratigraphic makeup, petrologic features such as microfractures and crystallites, and highly fractionated geochemistry indicate that this unit had a high viscosity and is most likely a ring fracture dome. Furthermore, radiogenic isotope ratios and the location along the ring fracture suggest that it formed as an extra-caldera rhyolitic dome, most comparable to the Roaring Mountain Member. From this we have determined that the source of the Dunraven Road flow is most likely from the extra-caldera side of the ring fracture. Figure 22 is a modified map of the Dunraven Road flow, based upon our field work. Of particular interest is that low-

δ18O feldspars and glass measurements by Hildreth et al. (1984) require the source rock had been hydrothermally altered.

The Dunraven Road flow may have been formed by assimilation of Archean crust and extensive fractional crystallization. The same model also can be used to model other extra-caldera rhyolites, excluding Cougar Creek and Riverside flows, which would require a higher equilibration temperature to achieve the radiogenic values (Hildreth et al., 1991; Nastanski, 2002). Using a one stage EC-RAxFC model requires the source rock to be approximately 0‰ to explain the δ18O value measured for Dunraven

Road flow, 5‰. Thus, the hydrothermally altered protolith in this case was most likely Archean rocks at upper crustal depths, indicating that fracture porosity and resulting hydrothermal alteration may extend to melting depths and transmit enough meteoric water to sufficiently lower δ18O values of the wall rock.

Figure 29. Generalized cartoon of development of UBM rhyolites, not to scale. Letters correspond to EC-RAxFC models. A - high amount of assimilation and fractional crystallization (low Teq), B - homogenized magma chamber, C- Small melt from the hydrothermally altered ring fracture (basalt dikes not presented on picture). Small boxes indicate fractional crystallization.

During assimilation it is assumed that the margins of the intrusion digested the most country rock and that plagioclase phenocrysts crystallizing in this region were possibly entrained in the eruptible magma, which also contains plagioclase phenocrysts in equilibrium with the glass values for 87Sr/86Sr, or the initial magma had slightly more radiogenic value, which was lowered by subsequent recharge. This seems more plausible for Dunraven Road flow as the measured plagioclase are generally only 0.0015

87Sr/86Sr higher than the glass, where as Tuff of Sulphur Creek and Canyon flow contain phenocrysts that are up to 0.0025 87Sr/86Sr higher than the glass values. However, it is also plausible that some mixing did occur prior to eruption.

Conclusions

The most significant conclusions of this work are summarized below.

1. The oldest members of the EUBM, the Tuff of Uncle Tom’s Trail and Tuff of Sulphur Creek are

most likely the same unit and were deposited as a pyroclastic density current based on field and

petrologic observations.

2. The Canyon flow is most likely composed of multiple flows, with at least one younger flow

exposed near the Silver Cord Falls area.

3. The youngest member of the EUBM is most likely an extra-caldera unit similar to the Roaring

Mountain Member and is the only known low-δ18O rhyolite erupted from outside the caldera

boundaries. The formation of the Dunraven Road flow can be best explained by a single EC-

RAxFC event assuming that hydrothermal alteration extended to depths along the ring fracture

zone.

4. Genesis of the Tuff of Sulphur Creek and Canyon flow involved the hydrothermal alteration of

the cooled margins of the larger magma chamber feeding the Yellowstone volcanic area,

modeled using EC-RAxFC, followed by subsidence and remelting following the collapse of the

current caldera.

Acknowledgments

Greatly appreciated field help was given by Allen Anderson, William Starkel, and Kevin Tarbert.

Sample analyses were conducted at Washington State University GeoAnalytical Laboratories. Sampling permits were issued by Yellowstone National Park, Research Permit Office, with help from Christie L.

Hendrix. We greatly appreciate discussions and 87Sr/86Sr values for the Scaup Lake flow from Dr. Jorge

Vazquez. Samples from the Biscuit Basin flows were from Dr. Ilya Bindeman and Kathryn Watts. This study was funded by NSF grant #EAR-0609475 and WSU SEES.

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APPENDIX A

WHOLE ROCK MAJOR AND TRACE ELEMENT DATA

Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Creek Creek Creek Creek Creek Creek

Locality Peter's Ridge Peter's Ridge Peter's Ridge Peter's Ridge Peter's Ridge Peter's Ridge northing 4952944 4952984 4952997 4953027 4953056 4953073 easting (12) 543026 542939 542937 542962 542941 542964 Lithology tuff tuff tuff tuff tuff tuff Source CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 Age (Ma) 0.479 0.479 0.479 0.479 0.479 0.479 Age error 0.01 0.01 0.01 0.01 0.01 0.01 Sample # 07CP01 07CP02 07CP03 O7CP04 07CP05 07CP06 Date 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 SiO2 76.19 76.63 76.12 76.32 76.07 75.97 TiO2 0.34 0.33 0.35 0.36 0.34 0.34 Al2O3 12.44 12.73 12.49 12.53 12.52 12.63 FeO* 1.77 1.38 1.92 1.68 2.02 1.95 MnO 0.02 0.02 0.03 0.03 0.03 0.02 MgO 0.07 0.09 0.05 0.05 0.07 0.05 CaO 0.69 0.58 0.65 0.67 0.66 0.67 Na2O 3.46 3.26 3.42 3.41 3.34 3.41 K2O 4.98 4.94 4.93 4.93 4.93 4.93 P2O5 0.04 0.04 0.03 0.03 0.03 0.04 Raw 96.54 95.49 96.59 96.48 96.28 96.29 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.00 0.00 0.00 0.00 0.00 0.00 Cr 2.60 3.80 2.90 3.20 4.20 2.50 Sc 5.10 5.90 5.30 5.50 5.20 5.50 V 3.30 1.70 4.70 1.40 3.40 2.50 Ba 996.60 971.60 1023.50 1021.10 989.00 1042.60 Rb 170.90 166.70 167.30 170.00 167.10 168.50 Sr 72.10 67.10 74.30 77.70 71.90 92.90 Zr 362.10 360.80 370.90 375.70 362.30 370.00 Y 44.60 56.00 58.00 54.60 47.20 50.70 Nb 47.60 47.50 47.50 47.90 47.30 48.00 Ga 20.10 19.50 20.70 20.00 20.70 20.80 Cu 0.70 1.80 0.20 0.40 -0.90 -1.40 Zn 73.60 56.80 67.50 71.10 65.00 34.60 Pb 39.00 35.90 35.20 58.40 32.30 32.70 La 57.50 69.30 73.60 75.30 58.00 70.80 Ce 104.70 134.50 136.80 149.20 136.10 110.40 Th 23.40 25.10 23.40 23.90 22.90 24.30 Nd 46.10 57.90 63.70 61.70 52.80 50.70 U 5.10 5.40 5.60 6.20 5.00 5.00

ICP-MS (ppm) La 63.84 74.52 77.75 78.90 63.13 78.94 Ce 110.90 143.72 139.07 153.89 139.47 118.05 Pr 13.50 16.78 17.58 17.40 14.56 15.19 Nd 48.52 61.33 64.30 63.40 53.32 54.62 Sm 9.92 12.72 13.48 13.23 11.20 11.04 Eu 1.90 2.04 1.98 2.00 1.98 1.96 Gd 8.76 11.67 12.16 11.89 10.01 9.85 Tb 1.54 1.99 2.09 2.02 1.71 1.66 Dy 9.39 12.08 12.54 11.91 10.23 10.16 Ho 1.88 2.34 2.41 2.32 2.00 1.98 Er 5.27 6.28 6.44 6.16 5.40 5.50 Tm 0.77 0.90 0.92 0.87 0.78 0.80 Yb 4.76 5.50 5.49 5.32 4.75 4.94 Lu 0.75 0.81 0.81 0.80 0.71 0.77 Ba 1039 1030 1065 1053 1020 1077 Th 24.29 24.09 23.91 23.82 23.55 24.09 Nb 49.34 49.03 49.00 49.16 48.58 48.46 Y 45.09 55.91 58.38 54.41 46.30 49.89 Hf 10.91 10.83 10.96 10.99 10.67 10.82 Ta 3.46 3.45 3.42 3.41 3.39 3.38 U 6.04 5.92 5.83 5.88 5.60 5.86 Pb 35.52 31.26 34.21 56.89 31.43 32.38 Rb 175.9 171.6 169.5 171.1 169.2 169.8 Cs 2.83 2.54 3.25 2.94 2.86 2.56 Sr 74.46 68.74 75.46 77.83 71.57 92.70 Sc 5.13 5.37 5.30 5.45 5.65 5.37 Zr 363 365 368 374 363 369

105 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Creek Creek Creek Canyon Flow Creek Creek

Locality Peter's Ridge Peter's Ridge Peter's Ridge Peter's Ridge N. of Sulphur Ck. N. of Sulphur Ck. northing 4953099 4953207 4953283 4953311 4956628 4956569 easting (12) 542954 542834 542852 542889 547209 547207 Lithology tuff tuff tuff tuff tuff vitrophyre Source CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 Age (Ma) 0.479 0.479 0.479 0.484 0.479 0.479 Age error 0.01 0.01 0.01 0.015 0.01 0.01 Sample # 07CP07 07CP08 07CP09 07CP10 07CP11 07CP12 Date 17-Dec-07 17-Dec-07 17-Dec-07 19-Dec-07 19-Dec-07 19-Dec-07 SiO2 75.98 76.08 76.02 75.98 77.92 76.90 TiO2 0.34 0.34 0.34 0.35 0.32 0.31 Al2O3 12.55 12.63 12.57 12.41 12.26 12.40 FeO* 1.97 1.83 1.90 2.03 0.51 1.40 MnO 0.02 0.02 0.02 0.03 0.01 0.03 MgO 0.05 0.07 0.04 0.10 0.03 0.05 CaO 0.67 0.66 0.66 0.74 0.53 0.56 Na2O 3.46 3.32 3.40 3.45 3.31 3.11 K2O 4.91 5.01 5.02 4.87 5.08 5.20 P2O5 0.04 0.03 0.03 0.04 0.03 0.04 Raw 96.53 96.66 96.46 96.38 96.74 94.57 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.00 0.00 0.00 0.00 0.00 0.00 Cr 3.00 3.60 1.50 3.50 3.50 2.30 Sc 6.30 5.80 5.40 6.30 4.20 3.80 V 2.40 5.20 3.30 3.10 0.10 2.50 Ba 987.90 999.70 1003.00 999.70 950.10 881.60 Rb 165.20 175.60 171.50 166.40 174.40 176.00 Sr 76.50 73.90 74.90 79.30 63.70 58.70 Zr 368.50 369.50 364.90 371.60 356.80 329.00 Y 57.80 42.20 51.30 53.60 62.00 64.30 Nb 47.80 47.40 48.40 48.00 49.30 48.80 Ga 19.90 19.30 20.70 19.60 19.10 20.30 Cu 0.40 0.90 0.60 1.20 0.20 0.30 Zn 69.50 67.30 65.70 77.10 22.50 54.30 Pb 31.30 28.30 28.90 33.20 29.30 31.70 La 67.40 61.10 60.80 68.80 73.60 88.70 Ce 138.60 108.50 137.80 130.90 147.00 179.80 Th 23.50 23.70 23.30 23.80 26.40 25.30 Nd 58.60 49.40 48.70 61.20 61.50 66.50 U 5.90 5.50 5.40 4.70 6.70 6.60

ICP-MS (ppm) La 72.37 63.45 64.48 74.56 79.12 95.04 Ce 139.91 111.02 140.70 133.04 152.34 189.43 Pr 16.53 13.81 13.84 16.98 17.93 20.96 Nd 60.52 50.42 49.88 62.47 67.27 71.73 Sm 12.65 10.35 10.34 12.91 13.91 14.08 Eu 1.99 2.00 1.92 1.95 1.93 1.55 Gd 11.45 9.01 9.22 11.63 12.82 12.48 Tb 1.95 1.54 1.59 1.96 2.13 2.09 Dy 11.82 9.24 9.82 11.64 12.73 12.66 Ho 2.31 1.80 2.01 2.23 2.51 2.52 Er 6.25 4.87 5.53 5.96 6.68 6.96 Tm 0.91 0.71 0.82 0.87 0.96 1.01 Yb 5.56 4.34 4.99 5.21 5.85 6.17 Lu 0.84 0.66 0.76 0.79 0.87 0.95 Ba 1020 1018 1032 1033 975 915 Th 23.46 23.32 23.72 23.26 25.35 25.10 Nb 48.72 48.07 49.25 48.74 51.11 50.19 Y 56.99 41.72 51.31 53.00 61.20 64.23 Hf 10.63 10.80 10.79 10.80 10.75 10.15 Ta 3.40 3.33 3.44 3.36 3.56 3.53 U 5.88 5.49 5.91 5.72 6.44 6.25 Pb 30.30 27.34 27.72 32.01 28.16 31.98 Rb 167.8 176.4 174.6 169.3 178.7 179.0 Cs 3.35 3.49 3.77 3.66 3.74 4.87 Sr 76.74 73.97 76.02 79.05 63.53 59.18 Sc 6.18 5.67 6.16 6.08 4.36 5.48 Zr 358 367 367 368 359 333

106 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Obsidian Creek Dunraven Road Dunraven Road Tuff of Sulphur Unit Canyon Flow Canyon Flow Flow Flow Creek Gardner River

Locality 7-mile hole trail 7-mile hole trail Dunraven Pass Dunraven Pass N. of Sulphur Ck. Gardner River northing 4954799 4953276 4955387 4955387 4956699 4971272 easting (12) 543870 543069 540434 540434 545734 521773 Lithology tuff tuff vitric picked glass alt. tuff rhyolite Source CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 Age (Ma) 0.484 0.484 0.486 0.486 0.479 0.3005 Age error 0.015 0.015 0.042 0.042 0.01 0.0028 Sample # 07CP13 07CP14 07CP15 07CP15-OBS 07CP16 GR-1-R Date 19-Dec-07 19-Dec-07 19-Dec-07 1-Mar-08 19-Dec-07 7-Jan-08 SiO2 75.84 75.93 77.59 77.49 80.17 74.12 TiO2 0.35 0.34 0.12 0.14 0.32 0.32 Al2O3 12.54 12.61 12.17 11.88 10.57 12.80 FeO* 2.19 1.96 0.88 1.22 0.99 2.53 MnO 0.03 0.04 0.02 0.03 0.03 0.04 MgO 0.04 0.08 0.04 0.12 0.04 0.61 CaO 0.66 0.66 0.47 0.56 0.37 1.58 Na2O 3.38 3.41 3.48 3.15 2.52 3.63 K2O 4.93 4.93 5.20 5.38 4.97 4.33 P2O5 0.04 0.03 0.02 0.02 0.02 0.04 Raw 96.09 96.74 96.73 100.30 93.54 97.47 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.00 0.00 0.00 0.00 0.00 9.75 Cr 2.90 2.80 2.40 1.00 2.10 18.00 Sc 6.10 6.40 2.80 3.80 3.40 5.60 V 2.50 4.60 -0.70 2.20 -0.30 30.70 Ba 1004.70 989.10 653.50 633.80 597.40 480.20 Rb 165.90 167.10 169.10 186.60 169.50 145.10 Sr 73.40 75.40 19.20 17.30 21.80 78.30 Zr 387.70 369.00 187.40 190.30 357.70 207.00 Y 60.50 54.00 48.00 53.20 59.20 61.00 Nb 48.00 48.30 33.90 34.40 48.90 29.70 Ga 20.30 20.80 20.50 19.00 16.10 22.20 Cu -0.10 1.60 -0.50 4.70 -0.10 19.60 Zn 65.00 71.40 40.60 51.90 47.40 83.30 Pb 27.40 37.60 33.80 33.50 32.20 24.30 La 70.00 71.00 58.30 59.00 66.10 65.30 Ce 134.30 144.90 108.60 114.70 126.00 125.30 Th 23.60 24.60 23.50 29.10 24.00 18.10 Nd 59.10 58.40 44.50 45.30 52.90 53.70 U 5.60 5.40 4.20 4.50 5.10 4.30

ICP-MS (ppm) La 75.26 76.67 60.39 62.21 71.89 66.01 Ce 139.91 150.57 111.95 119.22 138.40 123.41 Pr 16.72 16.78 12.80 13.45 15.57 14.26 Nd 61.32 60.29 45.68 48.29 55.86 52.60 Sm 12.77 12.52 9.49 10.15 11.54 11.47 Eu 1.93 1.89 0.69 0.66 0.84 1.03 Gd 11.64 11.01 8.78 9.36 10.64 11.16 Tb 1.98 1.91 1.50 1.60 1.82 1.89 Dy 11.97 11.43 9.19 9.80 11.37 11.62 Ho 2.38 2.26 1.82 1.96 2.27 2.33 Er 6.42 6.13 4.92 5.30 6.33 6.09 Tm 0.93 0.89 0.72 0.77 0.94 0.87 Yb 5.71 5.44 4.35 4.73 5.74 5.18 Lu 0.87 0.82 0.66 0.72 0.89 0.76 Ba 1032 1019 671 643 621 483 Th 23.48 23.67 23.07 20.36 23.94 18.36 Nb 49.30 49.14 34.24 33.33 50.19 30.60 Y 60.04 53.24 47.02 50.33 59.19 59.63 Hf 10.98 10.80 7.06 6.97 10.96 7.38 Ta 3.40 3.44 2.54 2.49 3.49 2.31 U 5.62 5.81 4.67 4.68 6.26 4.38 Pb 27.22 37.39 32.10 30.98 31.65 24.80 Rb 168.9 170.1 172.4 185.9 174.9 148.5 Cs 2.73 3.69 3.27 3.41 4.00 1.95 Sr 74.37 76.06 19.28 15.47 23.05 79.21 Sc 6.38 6.35 3.44 3.70 4.29 5.09 Zr 374 367 192 187 364 207

107 Member Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek

Unit Gardner River Gardner River Gardner River Gardner River Gardner River Gardner River

Locality Gardner River Gardner River Gardner River Gardner River Gardner River Gardner River northing 4971272 4971272 4971272 4971343 4971343 4971343 easting (12) 521773 521773 521773 521986 521986 521986 Lithology basalt rhyolite basalt rhyolite basalt basalt Source CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 Age (Ma) 0.3005 0.3005 0.3005 0.3005 0.3005 0.3005 Age error 0.0028 0.0028 0.0028 0.0028 0.0028 0.0028 Sample # GR-1-B GR-2-R GR-2-B GR-3-R GR-3-B GR-3-2-B Date 7-Jan-08 7-Jan-08 7-Jan-08 7-Jan-08 7-Jan-08 7-Jan-08 SiO2 54.77 76.74 66.24 77.04 64.74 57.33 TiO2 1.39 0.15 0.81 0.13 0.82 1.34 Al2O3 15.39 12.27 14.19 12.13 13.98 15.38 FeO* 9.02 1.58 5.08 1.54 5.63 8.17 MnO 0.14 0.01 0.08 0.01 0.09 0.12 MgO 6.20 0.10 2.30 0.03 3.37 4.83 CaO 8.71 0.56 4.77 0.54 5.11 7.89 Na2O 3.04 3.76 3.55 3.75 3.43 3.35 K2O 1.16 4.81 2.89 4.82 2.73 1.40 P2O5 0.17 0.03 0.10 0.02 0.11 0.17 Raw 98.26 97.20 98.11 97.15 98.22 98.15 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 95.66 4.17 24.01 0.00 50.50 65.92 Cr 98.90 3.90 54.40 3.30 55.80 92.10 Sc 22.70 2.60 13.30 1.50 14.30 21.70 V 189.00 7.20 99.70 1.60 105.20 176.60 Ba 293.90 481.70 395.50 463.70 370.20 327.90 Rb 34.00 162.70 97.70 163.30 93.50 46.40 Sr 349.30 30.60 198.30 24.30 205.60 312.10 Zr 124.60 208.40 181.20 205.70 166.50 147.70 Y 28.40 46.80 49.60 48.50 42.90 41.40 Nb 13.20 31.50 24.10 31.60 22.10 16.60 Ga 19.00 21.30 20.70 21.50 20.70 19.90 Cu 39.30 7.80 16.90 2.10 27.30 15.40 Zn 91.20 50.80 96.30 56.30 90.30 123.30 Pb 5.30 27.70 20.50 23.50 17.10 13.50 La 24.30 63.10 48.50 68.20 43.30 42.20 Ce 44.40 106.30 86.70 99.90 84.50 68.10 Th 4.10 20.00 11.00 19.90 11.20 5.00 Nd 21.80 50.00 41.00 53.30 38.80 39.90 U 1.50 4.20 2.70 2.90 1.80 0.90

ICP-MS (ppm) La 22.17 66.36 49.23 71.34 42.49 41.81 Ce 44.76 114.20 90.04 105.21 82.65 70.01 Pr 5.61 14.55 11.22 15.16 9.78 10.49 Nd 22.92 52.75 42.80 55.85 37.26 40.60 Sm 5.51 11.23 9.63 11.73 8.28 9.32 Eu 1.50 0.91 1.28 0.88 1.21 1.50 Gd 5.71 10.18 9.53 10.47 8.00 8.98 Tb 0.96 1.73 1.64 1.75 1.40 1.53 Dy 5.79 10.30 9.99 10.15 8.55 8.99 Ho 1.14 1.96 1.97 1.91 1.69 1.71 Er 2.96 5.13 5.17 4.89 4.45 4.40 Tm 0.41 0.73 0.73 0.67 0.63 0.62 Yb 2.46 4.32 4.39 3.97 3.82 3.75 Lu 0.36 0.61 0.65 0.57 0.56 0.54 Ba 291 496 400 474 366 323 Th 4.20 21.20 12.80 20.13 11.38 6.03 Nb 13.84 33.23 25.55 32.59 22.77 17.08 Y 29.03 46.78 49.35 46.81 42.79 41.46 Hf 3.64 7.79 6.12 7.67 5.56 4.35 Ta 0.94 2.57 1.84 2.53 1.67 1.17 U 1.00 4.21 3.06 3.85 2.64 1.55 Pb 5.98 29.11 21.46 23.96 18.26 13.45 Rb 34.8 168.7 102.6 164.0 93.6 46.6 Cs 0.50 1.97 1.47 1.91 1.52 0.67 Sr 359.22 32.46 203.25 25.43 206.97 316.01 Sc 22.30 2.19 13.50 1.70 12.70 19.27 Zr 121 214 183 205 163 142

108 Member Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek Upper Basin Dunraven Road Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Flow

Locality Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake northing 4962689 4962689 4962689 4962689 4962689 4955840 easting (12) 518948 518948 518948 518948 518948 542283 Lithology rhyolite basalt spherulite rhyolite basalt obsidian Source CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 08 Age (Ma) 0.2633 0.2633 0.2633 0.2633 0.2633 0.486 Age error 0.0034 0.0034 0.0034 0.0034 0.0034 0.042 Sample # GL-4-R GL-4-B GL-5-L GL-5-R GL-5-B 08CP01 Date 7-Jan-08 7-Jan-08 7-Jan-08 7-Jan-08 8-Jan-08 27-Dec-08 SiO2 76.62 61.36 77.33 77.39 61.70 77.34 TiO2 0.14 1.09 0.10 0.10 1.07 0.13 Al2O3 12.19 14.47 12.17 12.05 14.59 12.09 FeO* 1.55 6.99 1.35 1.33 6.89 1.18 MnO 0.04 0.15 0.03 0.03 0.13 0.03 MgO 0.21 4.35 0.03 0.02 4.26 0.07 CaO 0.68 6.18 0.30 0.44 6.04 0.53 Na2O 3.49 3.51 3.84 3.74 3.50 3.49 K2O 5.06 1.78 4.84 4.88 1.67 5.13 P2O5 0.02 0.14 0.02 0.01 0.15 0.01 Raw 96.78 98.27 97.88 97.47 96.41 98.88 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.94 46.47 0.00 0.00 46.32 0.13 Cr 3.90 49.40 3.00 1.00 49.90 4.00 Sc 1.10 18.70 2.20 2.30 17.40 4.30 V 5.30 136.00 3.10 1.00 125.60 1.60 Ba 236.90 290.00 104.50 99.80 302.00 654.10 Rb 184.20 43.30 191.40 191.90 34.00 168.30 Sr 21.30 220.00 8.10 7.70 215.00 20.40 Zr 188.50 155.60 195.80 192.60 156.70 186.40 Y 57.00 57.20 47.50 67.00 52.00 52.00 Nb 32.80 21.50 36.70 36.80 20.80 33.30 Ga 22.40 21.40 22.40 23.50 20.80 19.00 Cu 5.50 15.10 2.30 2.10 16.90 0.00 Zn 70.60 103.50 68.70 76.50 99.10 51.30 Pb 31.10 32.30 33.20 35.00 21.40 30.60 La 61.90 54.80 69.60 63.80 46.10 60.40 Ce 119.70 92.90 143.30 123.80 89.90 117.30 Th 21.50 9.00 24.80 24.00 9.70 21.00 Nd 49.50 47.90 54.20 53.40 42.30 45.60 U 4.90 2.70 6.20 6.10 1.80 4.70

ICP-MS (ppm) La 65.72 52.04 74.15 64.97 46.38 62.52 Ce 124.10 93.21 146.63 126.53 94.02 119.12 Pr 13.98 12.64 15.99 14.61 11.43 13.39 Nd 50.47 48.44 56.40 53.76 43.64 48.38 Sm 10.90 10.91 12.21 12.03 9.97 10.15 Eu 0.60 1.32 0.43 0.43 1.23 0.72 Gd 10.28 10.60 10.66 11.71 9.92 9.32 Tb 1.80 1.84 1.93 2.08 1.72 1.58 Dy 11.09 11.24 11.64 12.73 10.56 9.71 Ho 2.20 2.19 2.24 2.54 2.08 1.95 Er 5.89 5.65 5.91 6.86 5.40 5.33 Tm 0.86 0.80 0.86 0.98 0.75 0.76 Yb 5.17 4.66 5.19 5.99 4.47 4.77 Lu 0.75 0.68 0.74 0.88 0.64 0.72 Ba 241 286 106 109 296 664 Th 21.71 10.25 24.11 23.65 11.30 20.14 Nb 33.42 21.61 37.57 37.48 22.12 33.45 Y 56.43 56.85 46.80 65.32 52.38 51.20 Hf 7.62 5.10 8.15 8.14 5.19 7.06 Ta 2.59 1.57 2.86 2.91 1.57 2.50 U 5.12 2.43 5.90 5.80 2.41 4.53 Pb 32.27 31.90 33.45 34.99 21.33 31.44 Rb 187.5 44.0 193.0 195.3 34.5 172.2 Cs 3.77 1.10 4.07 4.29 1.04 3.38 Sr 22.48 222.14 9.85 10.05 218.06 20.14 Sc 2.05 16.80 1.39 1.41 16.52 4.00 Zr 192 149 197 197 148 191

109 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Dunraven Road Dunraven Road Dunraven Road Dunraven Road Dunraven Road Unit Flow Flow Flow Flow Canyon Flow Flow

Locality northing 4955445 4955321 4954982 4954966 4955312 4955491 easting (12) 542131 542127 542321 542541 542242 542200 Lithology wx tuff vitric obsidian wx obsidian tuff tuff Source CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 Age (Ma) 0.486 0.486 0.486 0.486 0.484 0.486 Age error 0.042 0.042 0.042 0.042 0.015 0.042 Sample # 08CP02 08CP03 08CP04 08CP05 08CP06 08CP07 Date 27-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 SiO2 77.62 77.54 77.53 76.87 75.79 77.74 TiO2 0.12 0.12 0.12 0.16 0.35 0.12 Al2O3 12.22 12.07 11.99 12.56 12.57 12.09 FeO* 1.01 1.23 1.12 1.30 1.95 0.99 MnO 0.01 0.02 0.03 0.03 0.08 0.01 MgO 0.03 0.03 0.05 0.06 0.11 0.02 CaO 0.36 0.35 0.48 0.51 0.76 0.34 Na2O 3.45 3.45 3.47 3.40 3.50 3.47 K2O 5.17 5.18 5.17 5.09 4.86 5.19 P2O5 0.02 0.01 0.01 0.02 0.03 0.02 Raw 99.51 99.81 99.09 98.53 99.42 99.67 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 1.39 2.70 0.68 0.00 0.88 0.86 Cr 3.70 2.10 1.50 2.80 3.70 2.70 Sc 3.80 3.40 5.00 3.90 6.10 2.50 V 0.80 0.50 2.30 1.80 5.00 0.00 Ba 657.90 675.20 658.60 715.10 1047.30 667.50 Rb 169.60 168.60 170.50 166.00 164.70 170.00 Sr 19.00 19.70 17.00 28.70 77.20 19.80 Zr 188.20 191.60 186.80 212.30 386.90 188.40 Y 45.40 42.80 51.90 47.90 61.80 47.00 Nb 33.80 34.40 33.10 36.10 49.90 34.70 Ga 19.40 18.80 18.40 20.80 20.70 19.80 Cu 0.00 0.40 0.10 0.10 1.20 0.00 Zn 32.70 40.60 51.30 50.80 84.00 35.50 Pb 26.70 29.70 30.10 30.50 31.50 26.30 La 55.10 49.80 60.70 59.30 80.80 64.50 Ce 93.40 117.80 118.80 121.70 157.10 169.80 Th 21.80 21.40 21.00 21.40 25.50 22.00 Nd 43.10 38.40 46.20 45.40 61.50 54.80 U 3.40 4.40 4.60 4.80 6.60 4.50

ICP-MS (ppm) La 55.30 49.46 62.23 63.24 79.75 68.52 Ce 91.75 120.71 119.52 120.82 155.50 170.32 Pr 12.56 11.10 13.42 13.08 17.52 16.01 Nd 44.76 39.61 48.38 46.64 63.92 58.24 Sm 9.57 8.53 10.09 9.57 13.12 12.25 Eu 0.73 0.68 0.69 0.85 1.96 0.74 Gd 8.24 7.30 9.15 8.65 11.61 10.50 Tb 1.43 1.29 1.59 1.49 1.98 1.75 Dy 8.75 8.11 9.77 9.19 12.25 10.36 Ho 1.73 1.60 1.96 1.83 2.41 1.87 Er 4.72 4.44 5.35 4.91 6.61 4.85 Tm 0.68 0.67 0.78 0.72 0.96 0.70 Yb 4.27 4.32 4.80 4.44 5.94 4.28 Lu 0.63 0.66 0.72 0.68 0.91 0.61 Ba 671 678 657 725 1053 674 Th 20.69 21.17 20.55 21.28 24.00 21.34 Nb 33.02 33.41 32.74 35.47 49.27 33.85 Y 44.69 41.11 50.89 46.07 60.38 45.72 Hf 7.07 6.98 6.93 7.61 11.25 6.95 Ta 2.53 2.51 2.46 2.65 3.46 2.50 U 4.08 4.38 4.59 4.75 6.20 4.47 Pb 27.29 29.96 31.13 31.60 31.31 26.14 Rb 170.3 168.2 170.0 165.5 166.0 171.3 Cs 2.27 2.31 3.40 3.65 3.50 2.84 Sr 19.35 19.96 17.42 27.77 78.41 19.59 Sc 3.83 3.50 3.75 3.94 6.22 3.58 Zr 190 191 187 213 385 191

110 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Dunraven Road Dunraven Road Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Flow Flow Creek Creek Creek Creek

top of N. of top of N. of top of N. of top of N. of Locality Sulphur Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. northing 4956017 4956314 4956402 4956461 4956461 4956461 easting (12) 542455 542310 546753 547171 547171 547171 Lithology tuff banded obsidian tuff tuff breccia tuff Source CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 Age (Ma) 0.486 0.486 0.479 0.479 0.479 0.479 Age error 0.042 0.042 0.01 0.01 0.01 0.01 Sample # 08CP08 08CP09 08CP10 08CP11 08CP12 08CP13 Date 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 SiO2 77.52 77.44 76.74 77.36 76.24 76.89 TiO2 0.12 0.12 0.33 0.31 0.38 0.33 Al2O3 12.16 12.06 12.62 12.47 13.12 12.97 FeO* 1.11 1.13 1.29 0.80 0.83 1.10 MnO 0.02 0.03 0.02 0.01 0.02 0.00 MgO 0.03 0.05 0.06 0.06 0.18 0.08 CaO 0.37 0.50 0.58 0.54 0.98 0.50 Na2O 3.49 3.49 3.30 3.31 3.55 3.18 K2O 5.17 5.16 5.02 5.12 4.67 4.90 P2O5 0.02 0.01 0.04 0.03 0.02 0.04 Raw 100.26 99.48 99.21 99.14 99.33 98.71 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 2.15 0.00 0.00 1.24 2.12 0.00 Cr 1.70 2.80 3.20 6.40 10.30 2.20 Sc 4.40 4.10 4.10 4.10 5.50 5.20 V 2.20 0.90 4.10 2.40 7.60 2.90 Ba 666.40 662.60 979.00 921.40 1152.20 1017.60 Rb 170.30 169.50 174.70 179.90 151.50 167.70 Sr 20.20 18.60 68.00 61.10 110.50 73.80 Zr 189.80 187.10 365.60 352.50 404.70 367.60 Y 46.70 52.50 57.60 59.40 54.40 74.80 Nb 33.70 33.30 50.30 50.80 46.50 48.80 Ga 18.70 18.80 20.40 20.60 21.50 20.90 Cu 0.20 0.00 0.00 0.00 1.20 0.00 Zn 50.00 51.60 45.60 30.70 31.10 55.60 Pb 38.40 34.10 35.10 23.40 25.30 31.70 La 52.50 62.50 84.90 74.00 71.50 87.80 Ce 109.20 119.80 171.40 140.30 133.90 166.50 Th 21.80 20.60 26.50 26.50 24.60 25.60 Nd 40.60 47.30 73.90 60.30 56.30 66.80 U 5.00 4.30 5.80 6.50 4.70 6.60

ICP-MS (ppm) La 56.51 62.58 89.21 75.84 72.76 89.58 Ce 112.64 119.97 167.67 144.87 136.01 164.09 Pr 12.08 13.53 20.45 17.19 16.01 18.56 Nd 42.82 48.53 74.79 62.24 57.86 67.32 Sm 8.91 10.13 14.81 12.96 11.98 13.74 Eu 0.71 0.70 1.93 1.72 2.31 2.11 Gd 7.86 9.21 12.57 11.44 10.41 12.85 Tb 1.42 1.59 2.02 1.93 1.74 2.20 Dy 9.10 9.88 11.95 11.85 10.67 13.75 Ho 1.84 1.97 2.29 2.36 2.12 2.76 Er 5.03 5.30 6.13 6.42 5.68 7.60 Tm 0.74 0.78 0.87 0.93 0.84 1.10 Yb 4.66 4.73 5.46 5.70 5.15 6.73 Lu 0.69 0.72 0.81 0.87 0.79 1.04 Ba 672 665 983 926 1163 1032 Th 20.63 20.41 23.86 25.04 22.36 23.61 Nb 31.99 33.22 49.63 49.90 46.05 48.29 Y 44.92 51.12 56.57 58.16 53.10 73.70 Hf 7.10 7.05 10.75 10.49 11.60 10.85 Ta 2.42 2.49 3.50 3.56 3.24 3.43 U 4.78 4.62 5.90 6.22 5.68 6.11 Pb 38.17 33.60 35.04 23.70 25.37 30.77 Rb 171.1 171.1 176.6 180.5 152.0 169.0 Cs 2.57 3.41 3.35 3.27 3.73 2.76 Sr 19.08 18.88 67.86 60.87 110.49 73.85 Sc 4.60 3.98 6.25 5.04 6.46 5.79 Zr 190 189 371 354 404 370

111 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Creek Creek Creek Creek Canyon Flow Canyon Flow

top of N. of top of N. of top of N. of Locality Sulphur Ck. Sulphur Ck. Sulphur Ck. S. Side of Canyon S. Side of Canyon S. Side of Canyon northing 4956553 4956553 4956666 4952198 4952305 4952454 easting (12) 547154 547154 547140 543104 543470 543589 Lithology breccia breccia breccia wx. Tuff tuff tuff Source CJP 08 CJP 08 CJP 08 CJP 08 CJP 09 CJP 08 Age (Ma) 0.479 0.479 0.479 0.479 0.484 0.479 Age error 0.01 0.01 0.01 0.01 0.015 0.01 Sample # 08CP14 08CP15 08CP16 08CP18 08CP19 08CP20 Date 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 SiO2 77.29 75.59 75.89 76.51 77.12 77.04 TiO2 0.32 0.41 0.36 0.31 0.21 0.25 Al2O3 12.51 13.29 12.77 12.29 12.14 12.24 FeO* 0.63 1.21 1.63 1.69 1.52 1.53 MnO 0.02 0.03 0.03 0.03 0.03 0.02 MgO 0.08 0.23 0.14 0.06 0.04 0.04 CaO 0.62 1.10 0.83 0.69 0.43 0.45 Na2O 3.42 3.54 3.47 3.42 3.30 3.26 K2O 5.07 4.57 4.82 4.98 5.19 5.14 P2O5 0.03 0.03 0.03 0.03 0.02 0.02 Raw 100.14 99.33 99.48 99.68 99.72 99.70 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 2.87 0.00 0.97 0.14 2.33 0.15 Cr 3.90 8.50 5.20 2.80 3.30 3.80 Sc 6.70 6.70 6.10 4.90 4.30 4.50 V 3.80 6.20 4.50 3.70 0.90 2.20 Ba 1002.00 1241.10 1073.80 962.60 799.00 859.70 Rb 175.70 147.10 162.70 175.50 174.40 176.80 Sr 71.00 125.10 85.70 66.90 38.30 49.30 Zr 363.50 432.10 393.50 349.70 270.60 290.90 Y 50.30 52.00 60.40 62.00 57.50 42.00 Nb 50.70 45.70 49.60 49.30 41.90 46.10 Ga 20.20 22.60 20.80 19.90 20.20 18.70 Cu 0.00 1.00 0.70 0.50 0.00 0.00 Zn 17.40 36.50 59.10 56.50 48.20 46.10 Pb 30.90 26.50 30.00 25.20 28.90 28.80 La 71.60 74.20 81.00 75.70 71.90 64.60 Ce 130.10 137.60 142.40 136.00 151.70 110.40 Th 26.50 22.30 24.80 24.80 24.80 25.00 Nd 52.90 55.30 61.00 58.70 59.80 46.20 U 6.80 6.20 7.20 6.00 7.00 6.40

ICP-MS (ppm) La 70.59 71.92 80.22 76.60 73.49 63.47 Ce 132.86 134.96 147.02 137.39 146.61 113.09 Pr 15.37 15.27 17.90 16.81 16.55 13.84 Nd 54.95 55.13 65.08 60.77 59.42 49.60 Sm 11.11 11.26 13.36 12.61 12.33 10.19 Eu 1.76 2.47 2.09 1.75 1.21 1.43 Gd 9.54 9.77 11.77 11.27 10.81 8.83 Tb 1.65 1.65 2.02 1.92 1.85 1.47 Dy 10.06 10.17 12.24 11.75 11.17 8.87 Ho 1.98 2.00 2.41 2.36 2.19 1.75 Er 5.44 5.49 6.44 6.41 5.90 4.79 Tm 0.82 0.81 0.94 0.93 0.85 0.69 Yb 5.16 4.97 5.78 5.75 5.35 4.36 Lu 0.78 0.77 0.86 0.88 0.78 0.67 Ba 1004 1257 1082 972 801 870 Th 24.94 21.27 23.22 24.21 23.13 23.30 Nb 50.07 45.64 49.13 48.63 40.61 45.08 Y 48.51 51.42 59.99 60.08 54.20 39.80 Hf 10.84 12.08 11.32 10.32 8.62 8.97 Ta 3.56 3.14 3.43 3.49 3.00 3.28 U 6.22 5.37 5.80 5.79 5.50 5.39 Pb 30.97 26.03 30.31 25.84 27.98 29.16 Rb 174.5 150.5 164.3 176.5 172.0 176.4 Cs 3.27 3.17 3.39 3.29 2.46 2.62 Sr 70.35 126.01 86.73 68.01 37.44 48.73 Sc 5.96 7.02 6.83 4.59 3.76 3.75 Zr 365 440 395 346 263 284

112 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin

Unit Canyon Flow Canyon Flow Canyon Flow Canyon Flow Canyon Flow Canyon Flow

Locality S. Side of Canyon S. Side of Canyon S. Side of Canyon S. Side of Canyon S. Side of Canyon S. Side of Canyon northing 4952592 4952592 4952592 4952622 4953147 4951779 easting (12) 543742 543742 543742 543804 544638 542020 Lithology tuff tuff tuff tuff tuff wx glass Source CJP 09 CJP 09 CJP 09 CJP 09 CJP 09 CJP 09 Age (Ma) 0.484 0.484 0.484 0.484 0.484 0.484 Age error 0.015 0.015 0.015 0.015 0.015 0.015 Sample # 08CP21A 08CP21B 08CP21C 08CP22 08CP23 08CP24 Date 28-Dec-08 28-Dec-08 29-Dec-08 29-Dec-08 29-Dec-08 29-Dec-08 SiO2 77.11 76.92 77.25 75.99 76.29 76.23 TiO2 0.19 0.23 0.19 0.31 0.34 0.34 Al2O3 12.14 12.15 12.13 12.45 12.41 12.86 FeO* 1.42 1.76 1.35 2.08 1.77 1.65 MnO 0.04 0.03 0.03 0.06 0.02 0.03 MgO 0.06 0.07 0.06 0.14 0.05 0.08 CaO 0.51 0.48 0.48 0.72 0.68 0.85 Na2O 3.38 3.29 3.33 3.42 3.43 2.39 K2O 5.14 5.04 5.17 4.80 4.96 5.55 P2O5 0.02 0.02 0.02 0.03 0.04 0.03 Raw 99.73 99.36 99.81 99.44 100.23 95.48 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 1.53 1.35 0.97 0.33 0.00 0.00 Cr 4.00 2.40 4.10 6.20 3.50 3.10 Sc 4.60 5.90 4.00 4.30 5.40 6.40 V 0.20 1.80 1.10 3.10 2.20 5.20 Ba 830.60 884.10 850.70 1021.00 1038.00 1028.40 Rb 171.00 170.80 173.60 162.50 174.00 195.60 Sr 38.40 49.80 39.90 77.70 79.00 86.80 Zr 239.30 273.20 237.20 330.40 382.20 372.90 Y 52.20 46.30 54.00 59.90 58.50 63.70 Nb 38.90 42.60 40.60 44.20 49.70 47.20 Ga 19.90 20.60 18.40 20.20 20.80 20.90 Cu 0.20 0.40 0.00 1.70 0.00 0.00 Zn 55.90 57.50 50.40 75.80 75.10 74.70 Pb 27.60 28.50 28.30 32.50 29.10 31.20 La 66.40 72.10 64.40 74.40 78.70 77.60 Ce 129.20 129.20 123.30 143.20 130.50 147.20 Th 21.70 23.20 23.30 22.80 24.90 24.00 Nd 49.60 52.00 48.90 55.50 60.40 58.20 U 4.80 5.70 5.30 6.20 5.50 5.70

ICP-MS (ppm) La 66.03 68.61 65.27 71.87 78.69 77.91 Ce 129.65 128.43 123.23 138.93 133.07 148.30 Pr 14.49 14.80 14.17 15.63 17.50 16.84 Nd 52.13 52.92 50.96 56.17 63.42 60.82 Sm 10.86 10.70 10.60 11.50 12.99 12.42 Eu 1.13 1.33 1.14 1.73 1.97 1.97 Gd 9.84 9.21 9.73 10.57 11.55 11.45 Tb 1.66 1.58 1.65 1.81 1.95 1.95 Dy 10.16 9.45 10.12 11.20 11.70 11.98 Ho 2.03 1.87 2.03 2.28 2.31 2.45 Er 5.47 4.95 5.57 6.24 6.19 6.77 Tm 0.80 0.73 0.82 0.91 0.88 1.00 Yb 4.91 4.49 5.09 5.72 5.35 6.15 Lu 0.75 0.68 0.77 0.87 0.80 0.95 Ba 833 891 850 1016 1037 1047 Th 21.83 22.28 22.18 21.77 23.73 23.02 Nb 37.63 41.35 39.30 42.97 48.09 47.89 Y 49.48 44.25 51.86 58.82 55.00 63.25 Hf 7.91 8.57 7.77 9.53 10.95 10.68 Ta 2.79 3.02 2.87 3.05 3.45 3.34 U 5.15 5.31 5.26 5.51 5.86 5.69 Pb 28.93 28.10 28.51 31.90 29.09 30.61 Rb 168.8 171.7 172.5 162.7 172.6 202.7 Cs 3.03 3.53 2.89 4.11 3.03 6.81 Sr 38.32 49.51 39.40 78.47 77.74 88.78 Sc 3.70 4.17 3.68 5.39 5.64 5.64 Zr 232 267 231 318 370 367

113 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Unit Canyon Flow Canyon Flow Canyon Flow Canyon Flow Creek Creek

paleo-valley S. basal ash flow, basal ash flow, Locality flow top breccia flow top breccia flow top breccia side of canyon N.of Sulphur Ck. N.of Sulphur Ck. northing 4951788 4951788 4951788 4951810 4956392 4956392 easting (12) 542030 542030 542030 542014 547242 547242 Lithology hydrated breccia pumice vitric vitric ignimbrite pumice Source CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 Age (Ma) 0.484 0.484 0.484 0.484 0.479 0.479 Age error 0.015 0.015 0.015 0.015 0.01 0.01 Sample # 08CP25A 08CP25B 08CP25C 08CP26 08CP27WR 08CP27P Date 29-Dec-08 29-Dec-08 29-Dec-08 29-Dec-08 29-Dec-08 29-Dec-08 SiO2 80.06 77.90 77.09 76.55 77.23 89.25 TiO2 0.31 0.33 0.32 0.34 0.33 0.16 Al2O3 11.35 12.57 12.39 12.64 12.68 6.07 FeO* 1.15 1.35 1.28 1.35 1.31 0.43 MnO 0.04 0.04 0.04 0.03 0.03 0.02 MgO 0.10 0.08 0.08 0.07 0.10 0.02 CaO 0.88 0.89 0.82 0.83 0.72 0.40 Na2O 1.74 1.78 2.08 2.50 2.71 1.16 K2O 4.36 5.02 5.88 5.65 4.88 2.49 P2O5 0.03 0.03 0.02 0.02 0.02 0.01 Raw 94.44 93.90 95.11 96.17 96.38 97.32 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.00 0.00 0.00 0.00 0.00 0.00 Cr 3.10 4.10 3.90 3.70 8.30 3.50 Sc 5.10 5.40 5.00 5.20 5.30 3.60 V 2.70 1.70 1.10 1.50 6.60 3.50 Ba 938.10 1037.80 994.10 1016.00 966.40 741.90 Rb 181.10 208.90 197.60 180.90 171.70 86.30 Sr 92.40 87.60 73.70 81.70 69.90 44.20 Zr 328.00 345.50 348.80 369.40 348.60 175.10 Y 54.80 59.10 62.70 65.30 61.00 31.10 Nb 41.70 46.10 48.10 47.90 46.50 23.40 Ga 17.50 19.10 19.60 20.50 19.70 10.10 Cu 0.20 0.00 0.60 0.00 0.00 0.00 Zn 63.10 55.20 55.50 58.00 58.50 40.90 Pb 28.50 30.10 30.40 30.60 30.60 13.90 La 68.40 69.90 73.20 78.80 70.50 36.10 Ce 125.50 139.40 140.40 145.20 138.60 73.30 Th 21.20 22.90 25.40 24.70 23.70 12.70 Nd 50.70 54.90 56.10 60.10 55.10 28.30 U 4.10 5.20 5.20 6.70 5.30 2.80

ICP-MS (ppm) La 69.01 73.28 76.56 78.43 74.13 37.64 Ce 128.48 141.46 146.34 150.32 140.96 71.59 Pr 14.72 15.90 16.51 17.00 15.77 8.09 Nd 52.73 57.91 59.86 61.35 56.08 29.20 Sm 10.62 11.92 12.27 12.65 11.38 5.85 Eu 1.78 1.92 1.84 1.91 1.62 0.93 Gd 9.73 10.91 11.09 11.63 10.59 5.45 Tb 1.64 1.86 1.92 1.96 1.83 0.93 Dy 10.13 11.21 11.87 12.12 11.36 5.70 Ho 2.09 2.25 2.39 2.44 2.32 1.17 Er 5.74 6.31 6.56 6.86 6.45 3.22 Tm 0.85 0.93 0.97 0.99 0.94 0.47 Yb 5.28 5.74 6.01 6.17 5.93 2.93 Lu 0.80 0.88 0.93 0.95 0.90 0.45 Ba 970 1067 1017 1034 984 745 Th 19.98 22.82 23.41 23.56 23.07 11.30 Nb 42.56 46.95 47.52 48.45 47.28 23.83 Y 53.53 58.99 61.77 63.83 60.79 30.69 Hf 9.53 10.25 10.41 10.75 10.31 5.37 Ta 2.93 3.30 3.33 3.41 3.32 1.66 U 4.61 5.36 5.79 5.85 5.50 2.82 Pb 28.16 30.24 30.65 30.86 30.36 13.82 Rb 188.9 219.9 205.0 186.6 177.1 92.0 Cs 12.53 9.39 5.40 5.94 9.26 4.31 Sr 93.98 91.05 75.50 83.05 71.48 45.72 Sc 5.48 5.14 5.02 5.74 5.76 3.04 Zr 330 352 354 372 351 186

114 Member Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Creek Creek Creek

basal ash flow, basal ash flow, basal ash flow, Locality N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. northing 4956392 4956392 4956392 easting (12) 547242 547242 547242 Lithology ignimbrite pumice ignimbrite Source CJP 08 CJP 08 CJP 08 Age (Ma) 0.479 0.479 0.479 Age error 0.01 0.01 0.01 Sample # 08CP28WR 08CP28P 08CP29WR Date 30-Dec-08 30-Dec-08 31-Dec-08 SiO2 77.19 88.65 83.18 TiO2 0.31 0.19 0.18 Al2O3 12.80 6.52 9.35 FeO* 1.22 0.44 0.75 MnO 0.03 0.02 0.02 MgO 0.08 0.00 0.03 CaO 0.69 0.41 0.50 Na2O 2.67 1.08 2.17 K2O 5.00 2.68 3.80 P2O5 0.02 0.01 0.01 Raw 95.89 95.35 96.64 Total 100.00 100.00 100.00

(ppm) Ni 0.00 2.97 0.00 Cr 5.80 4.60 3.00 Sc 4.90 2.60 3.80 V 6.20 1.90 2.60 Ba 939.00 783.30 847.40 Rb 174.70 94.60 126.90 Sr 65.70 44.50 44.30 Zr 329.90 192.50 195.80 Y 59.50 34.50 43.60 Nb 45.80 25.10 31.40 Ga 20.50 9.60 15.10 Cu 0.00 0.00 0.00 Zn 61.00 34.90 43.60 Pb 28.40 13.10 20.70 La 69.80 44.80 51.70 Ce 133.80 77.30 98.40 Th 23.80 14.00 17.30 Nd 52.60 28.80 38.00 U 5.00 3.70 3.30

ICP-MS (ppm) La 71.89 41.64 51.07 Ce 136.69 80.30 97.82 Pr 15.30 9.11 11.08 Nd 54.75 33.04 40.00 Sm 11.21 6.81 8.26 Eu 1.59 0.99 1.13 Gd 10.22 6.14 7.60 Tb 1.78 1.06 1.30 Dy 11.10 6.48 8.15 Ho 2.26 1.30 1.64 Er 6.33 3.55 4.63 Tm 0.93 0.52 0.66 Yb 5.82 3.19 4.15 Lu 0.89 0.49 0.63 Ba 959 812 861 Th 22.49 12.14 16.02 Nb 47.09 26.27 31.57 Y 60.67 33.71 43.48 Hf 9.96 5.76 6.30 Ta 3.24 1.78 2.21 U 5.36 2.98 3.88 Pb 28.48 14.17 21.06 Rb 186.3 102.0 135.3 Cs 7.39 6.03 6.55 Sr 68.39 46.45 46.65 Sc 6.33 3.31 3.93 Zr 341 206 202

115 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Creek Creek Creek Creek Creek Creek

basal ash flow, basal ash flow, basal ash flow, basal ash flow, basal ash flow, basal ash flow, Locality N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. northing 4956392 4956392 4956392 4956392 4956392 4956392 easting (12) 547242 547242 547242 547242 547242 547242 Lithology pumice glass pumice ignimbrite pumice ignimbrite Source CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 Age (Ma) 0.479 0.479 0.479 0.479 0.479 0.479 Age error 0.01 0.01 0.01 0.01 0.01 0.01 Sample # 08CP29P 08CP30G 08CP30P 08CP31WR 08CP31P 08CP32WR Date 31-Dec-08 31-Dec-08 31-Dec-08 31-Dec-08 1-Jan-09 1-Jan-09 SiO2 82.56 77.65 84.29 76.91 89.56 76.95 TiO2 0.24 0.12 0.17 0.27 0.11 0.33 Al2O3 9.95 11.99 9.13 13.16 6.03 12.97 FeO* 0.69 1.12 0.68 1.28 0.29 1.16 MnO 0.03 0.03 0.02 0.03 0.01 0.03 MgO 0.04 0.04 0.04 0.06 0.00 0.05 CaO 0.65 0.45 0.42 0.62 0.27 0.77 Na2O 1.90 3.28 1.50 2.71 0.96 2.73 K2O 3.93 5.31 3.72 4.93 2.75 4.98 P2O5 0.01 0.01 0.01 0.02 0.01 0.02 Raw 95.37 98.10 94.68 95.21 95.72 95.68 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 2.28 0.12 0.87 0.00 5.29 0.00 Cr 3.70 3.80 3.90 4.60 2.60 5.00 Sc 2.80 4.20 3.60 5.90 2.40 5.50 V 5.40 0.00 5.60 16.60 0.30 5.80 Ba 1055.60 639.30 800.40 955.70 513.30 910.10 Rb 129.30 179.70 128.60 167.30 98.30 173.40 Sr 70.10 15.10 38.40 56.30 22.10 68.50 Zr 251.30 188.90 174.60 287.80 116.10 351.00 Y 47.40 51.50 45.90 52.90 30.60 59.50 Nb 35.20 33.00 30.50 41.90 21.90 47.70 Ga 15.10 19.40 14.80 19.30 9.70 20.60 Cu 0.00 0.00 0.00 0.00 0.00 0.00 Zn 45.30 52.90 52.50 69.90 35.60 66.30 Pb 18.90 30.10 17.20 27.40 13.70 27.40 La 59.70 63.40 51.30 64.50 37.80 72.50 Ce 102.40 114.40 102.20 119.80 69.80 131.80 Th 19.00 21.50 16.90 21.70 13.30 24.10 Nd 41.40 45.40 39.60 46.50 27.10 51.90 U 4.70 4.90 4.10 5.90 2.20 5.50

ICP-MS (ppm) La 57.89 63.27 52.02 62.02 35.95 69.60 Ce 110.50 121.72 101.81 119.25 69.38 133.34 Pr 12.55 13.71 11.60 13.21 7.84 15.06 Nd 45.41 48.97 42.05 47.61 27.91 54.51 Sm 9.13 10.25 8.65 9.77 5.72 11.15 Eu 1.57 0.70 0.99 1.35 0.60 1.61 Gd 8.60 9.39 8.28 9.30 5.34 10.43 Tb 1.50 1.66 1.45 1.59 0.92 1.82 Dy 9.08 10.01 8.70 9.84 5.64 11.23 Ho 1.84 2.02 1.75 2.02 1.15 2.28 Er 5.03 5.40 4.84 5.61 3.12 6.40 Tm 0.74 0.80 0.72 0.83 0.47 0.95 Yb 4.58 4.88 4.43 5.14 2.85 5.85 Lu 0.71 0.74 0.68 0.79 0.44 0.91 Ba 1100 664 833 987 525 934 Th 17.87 21.07 16.64 21.75 11.93 23.18 Nb 36.47 34.94 31.42 42.94 22.03 48.25 Y 47.56 52.26 46.42 52.12 29.65 60.56 Hf 7.74 7.07 6.08 9.10 4.01 10.49 Ta 2.58 2.56 2.30 3.07 1.58 3.36 U 4.33 4.72 4.00 5.04 2.84 5.65 Pb 19.38 31.31 17.75 28.50 13.22 28.06 Rb 134.7 185.0 134.3 169.5 101.9 177.0 Cs 5.61 3.73 6.60 6.69 5.80 8.29 Sr 71.77 16.44 40.47 56.98 23.47 71.37 Sc 3.93 4.01 4.04 5.64 2.32 5.79 Zr 263 195 185 294 122 358

116 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Tuff of Sulphur Unit Creek Creek Creek Creek Creek Creek

basal ash flow, basal ash flow, basal ash flow, basal ash flow, lower stoney lower stoney Locality N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. N.of Sulphur Ck. interior interior northing 4956392 4956398 4956400 4956400 4956404 4956428 easting (12) 547242 547247 547245 547245 547269 547312 Lithology pumice tuff vitrophyre vitrophyre tuff tuff Source CJP 08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 0.479 0.479 0.479 0.479 0.479 0.479 Age error 0.01 0.01 0.01 0.01 0.01 0.01 Sample # 08CP32P 08CP33 08CP34 08CP35 08CP36 08CP37 Date 1-Jan-09 1-Jan-09 1-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 SiO2 77.44 76.50 76.58 76.99 77.26 77.26 TiO2 0.33 0.34 0.31 0.30 0.33 0.35 Al2O3 12.86 13.42 12.37 12.32 12.77 12.71 FeO* 0.99 1.33 1.71 1.41 0.74 0.61 MnO 0.03 0.03 0.04 0.03 0.02 0.00 MgO 0.09 0.07 0.06 0.04 0.05 0.04 CaO 0.71 0.77 0.67 0.58 0.56 0.60 Na2O 2.35 2.71 3.06 3.11 3.23 3.37 K2O 5.18 4.79 5.18 5.18 5.03 5.02 P2O5 0.02 0.02 0.02 0.02 0.03 0.04 Raw 95.01 94.59 95.86 96.88 97.54 99.17 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 1.46 0.00 1.31 0.45 0.00 1.02 Cr 4.90 7.90 4.50 4.10 3.20 4.40 Sc 4.90 7.00 5.60 5.30 5.70 5.60 V 3.90 10.00 3.70 2.40 3.40 3.50 Ba 925.40 883.50 864.10 898.30 970.30 995.60 Rb 178.00 168.20 176.40 177.20 171.50 175.80 Sr 63.30 75.20 56.60 54.70 65.50 67.70 Zr 332.80 353.40 340.00 335.60 367.60 388.40 Y 60.90 55.70 67.30 63.80 61.40 71.00 Nb 47.80 46.00 49.10 48.70 50.10 50.90 Ga 20.10 19.70 18.80 18.90 19.90 21.50 Cu 0.60 0.70 0.70 0.00 0.00 0.90 Zn 57.40 74.50 66.70 58.50 35.70 26.20 Pb 24.90 19.80 31.20 31.10 32.00 31.00 La 73.30 66.20 80.80 80.70 78.50 94.40 Ce 135.00 125.00 157.20 158.00 166.40 193.40 Th 23.80 23.90 24.60 25.40 27.10 26.90 Nd 53.60 50.50 64.30 62.40 64.60 77.40 U 6.30 5.00 6.90 4.40 5.20 5.60

ICP-MS (ppm) La 72.68 68.16 81.25 83.18 81.48 94.80 Ce 139.26 128.85 159.94 161.83 165.13 193.80 Pr 15.73 14.58 18.49 18.44 18.71 22.19 Nd 56.42 52.18 67.40 65.41 67.53 81.32 Sm 11.44 10.69 13.97 13.21 13.97 16.80 Eu 1.56 1.61 1.67 1.54 1.88 1.98 Gd 10.58 9.78 12.46 11.88 12.26 15.15 Tb 1.85 1.71 2.15 2.05 2.12 2.57 Dy 11.35 10.45 12.98 12.40 12.64 14.83 Ho 2.31 2.14 2.57 2.50 2.49 2.89 Er 6.41 5.87 7.02 6.75 6.78 7.37 Tm 0.95 0.87 1.04 0.99 0.98 1.06 Yb 5.84 5.40 6.41 6.09 6.01 6.35 Lu 0.91 0.84 0.99 0.94 0.93 0.93 Ba 961 914 889 910 998 1020 Th 23.49 22.66 24.68 25.40 25.18 25.17 Nb 48.75 47.45 49.74 50.15 50.81 51.20 Y 60.85 56.28 67.46 63.74 61.30 69.52 Hf 10.30 10.57 10.32 10.24 11.03 11.05 Ta 3.42 3.30 3.46 3.55 3.54 3.57 U 5.78 5.32 6.09 6.16 6.23 6.64 Pb 25.96 21.01 31.29 31.94 31.66 30.30 Rb 184.1 171.1 179.0 180.7 175.0 178.1 Cs 8.20 8.99 4.97 4.79 3.57 2.66 Sr 64.85 77.09 57.87 55.91 66.67 67.77 Sc 5.45 6.94 5.72 5.33 5.63 5.83 Zr 343 359 346 341 378 383

117 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Tuff of Sulphur Tuff of Sulphur Unit Canyon Flow Creek Creek Canyon Flow Canyon Flow Canyon Flow

Locality 7-mile hole trail N. Canyon rim N. Canyon rim N. Canyon rim N. Canyon rim N. Canyon rim northing 4952902 4953445 4953445 4953835 4953840 4953094 easting (12) 542534 543881 543881 544298 544277 542915 Lithology wx glass tuff tuff tuff wx glass wx tuff Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 0.484 0.479 0.479 4.84 0.484 4.84 Age error 0.015 0.01 0.01 0.01 0.015 0.01 Sample # 08CP38 08CP39 08CP40 08CP41 08CP42 08CP43 Date 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 SiO2 76.15 76.03 75.97 76.28 75.96 75.92 TiO2 0.35 0.35 0.35 0.32 0.35 0.33 Al2O3 13.10 12.56 12.69 12.60 12.51 12.58 FeO* 2.04 1.93 1.84 1.69 1.91 1.99 MnO 0.04 0.02 0.02 0.03 0.04 0.03 MgO 0.07 0.03 0.04 0.04 0.07 0.06 CaO 0.82 0.66 0.66 0.72 0.79 0.72 Na2O 2.00 3.39 3.41 3.44 2.96 3.47 K2O 5.40 4.99 5.00 4.87 5.37 4.88 P2O5 0.03 0.03 0.03 0.02 0.04 0.03 Raw 94.62 98.80 98.32 98.68 96.26 98.55 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 1.38 0.34 0.01 0.08 0.90 0.21 Cr 2.80 3.10 3.30 3.90 3.70 3.10 Sc 6.40 5.90 5.40 3.50 5.90 5.80 V 4.50 3.60 4.00 3.80 4.10 2.00 Ba 984.20 1064.00 1081.50 1019.20 1001.50 1020.10 Rb 178.70 171.20 168.90 167.60 182.50 166.20 Sr 77.00 75.30 78.10 79.20 75.00 78.10 Zr 369.80 375.40 379.10 357.90 366.90 366.80 Y 166.20 62.50 46.60 58.60 63.90 56.50 Nb 49.00 49.00 48.50 48.50 48.00 48.70 Ga 20.50 20.50 21.20 20.80 19.70 20.80 Cu 0.60 0.50 0.80 0.00 0.00 0.00 Zn 76.50 56.80 70.20 58.20 78.80 72.20 Pb 30.40 30.40 29.30 29.90 30.10 28.60 La 80.60 75.90 71.20 77.80 77.70 74.60 Ce 157.80 146.80 135.60 156.00 151.20 145.30 Th 25.10 25.30 23.80 23.70 23.80 24.80 Nd 75.90 63.80 56.70 62.50 61.00 57.10 U 6.10 4.60 4.20 6.30 6.20 7.00

ICP-MS (ppm) La 84.58 77.20 74.40 80.70 81.52 73.96 Ce 168.88 150.39 137.55 154.47 156.87 146.64 Pr 20.34 18.02 16.36 17.76 17.94 16.19 Nd 81.10 66.12 58.91 64.08 65.20 58.73 Sm 19.48 13.90 12.06 13.11 13.36 12.15 Eu 4.27 1.95 1.98 2.01 1.89 1.93 Gd 24.23 12.48 10.38 11.70 12.04 10.98 Tb 4.24 2.12 1.76 2.00 2.07 1.85 Dy 26.62 12.68 10.42 11.88 12.49 11.15 Ho 5.68 2.49 1.99 2.37 2.51 2.30 Er 15.41 6.67 5.28 6.39 6.83 6.20 Tm 2.13 0.97 0.75 0.93 0.98 0.90 Yb 12.26 5.90 4.63 5.73 6.08 5.55 Lu 1.87 0.90 0.70 0.86 0.93 0.85 Ba 1023 1084 1108 1043 1035 1033 Th 24.49 24.24 23.74 23.84 23.96 23.58 Nb 49.99 49.40 49.42 48.91 49.39 48.86 Y 167.92 62.49 46.07 58.58 64.51 55.65 Hf 10.87 11.01 11.12 10.53 10.95 10.68 Ta 3.47 3.41 3.41 3.37 3.41 3.44 U 6.46 5.80 5.14 5.98 5.96 5.91 Pb 31.91 30.75 28.74 30.41 31.06 29.09 Rb 184.5 173.9 172.6 169.8 186.3 168.0 Cs 4.44 2.73 3.00 3.74 5.15 3.76 Sr 79.53 76.15 78.89 80.12 76.95 79.08 Sc 6.51 5.95 6.18 5.25 6.29 6.21 Zr 373 374 385 360 374 363

118 Basalt of Snake Basalt of Snake Member Upper Basin River River Messa Falls Tuff Messa Falls Tuff Messa Falls Tuff Basalt of Snake Basalt of Snake Unit Canyon Flow River River Messa Falls Tuff Messa Falls Tuff Messa Falls Tuff

along Hwy N of along Hwy N of along Hwy N of Locality 7-mile hole trail Island Park Island Park Ashton Ashton Ashton northing 4952962 4901868 4901846 4900273 4899626 4891167 easting (12) 542596 457412 457381 455909 455807 456941 Lithology wx glass tuff tuff ignimbrite ignimbrite ignimbrite Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 0.484 1.292 1.292 1.292 Age error 0.015 0.005 0.005 0.005 Sample # 08CP44 08CP45 08CP46 08CP47 08CP48 08CP49WR Date 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 SiO2 76.17 63.32 63.22 76.06 76.85 78.59 TiO2 0.36 0.62 0.62 0.20 0.19 0.11 Al2O3 13.23 16.08 16.10 12.71 12.25 11.74 FeO* 2.03 6.96 7.05 1.93 1.68 1.10 MnO 0.04 0.19 0.19 0.04 0.01 0.02 MgO 0.04 0.46 0.46 0.03 0.00 0.05 CaO 0.64 2.95 2.93 0.45 0.32 0.35 Na2O 2.48 4.69 4.71 3.48 3.45 2.98 K2O 4.98 4.55 4.55 5.07 5.22 5.03 P2O5 0.02 0.16 0.17 0.03 0.04 0.01 Raw 94.86 98.43 98.49 97.67 98.28 98.42 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.15 2.59 0.24 0.00 0.00 0.00 Cr 2.40 2.60 1.80 1.70 2.10 3.00 Sc 5.40 17.60 19.00 3.10 3.00 1.90 V 2.20 0.80 0.00 0.00 0.00 0.00 Ba 932.80 2772.50 2899.70 1015.20 973.10 189.00 Rb 165.90 131.70 124.80 143.40 178.20 205.80 Sr 68.00 151.00 156.40 26.60 22.80 12.80 Zr 381.30 1451.50 1470.10 359.10 352.80 143.60 Y 59.70 118.40 123.30 64.60 47.60 42.00 Nb 49.20 135.50 136.80 45.90 44.00 40.60 Ga 20.90 30.70 28.00 22.60 22.10 18.80 Cu 1.90 8.50 6.50 1.80 2.40 1.20 Zn 70.10 195.80 201.30 102.20 75.50 43.40 Pb 31.10 32.40 30.90 35.60 28.60 28.30 La 78.50 166.70 162.50 94.30 70.80 67.20 Ce 148.20 294.90 313.80 156.00 113.70 131.90 Th 26.40 21.30 21.50 29.60 27.10 30.30 Nd 58.90 123.40 124.60 67.60 48.70 43.30 U 4.90 4.90 5.30 5.20 5.50 6.70

ICP-MS (ppm) La 80.34 176.76 171.21 94.20 69.54 64.74 Ce 152.94 300.29 313.63 155.67 116.50 133.06 Pr 17.15 36.04 35.18 19.68 14.23 13.00 Nd 61.31 129.57 126.57 70.12 50.49 44.25 Sm 12.36 25.34 25.08 13.91 10.20 9.30 Eu 1.70 6.21 6.12 1.59 1.49 0.53 Gd 11.17 23.23 23.25 12.56 9.31 8.48 Tb 1.87 3.89 3.91 2.11 1.58 1.48 Dy 11.50 23.53 23.81 12.57 9.64 9.04 Ho 2.33 4.81 4.93 2.56 1.98 1.78 Er 6.37 13.47 13.59 6.80 5.40 4.94 Tm 0.94 1.98 2.02 0.98 0.80 0.76 Yb 5.83 12.46 12.73 5.94 4.86 4.88 Lu 0.89 1.98 2.02 0.86 0.74 0.72 Ba 968 2827 2954 1044 988 194 Th 24.89 19.51 19.64 27.56 26.69 29.54 Nb 50.69 136.55 137.00 45.73 44.08 40.34 Y 59.81 119.97 123.68 62.79 46.96 40.25 Hf 11.38 31.30 31.45 11.17 10.72 6.00 Ta 3.54 7.56 7.65 3.26 3.10 3.26 U 5.93 4.80 4.76 5.58 5.19 6.60 Pb 32.01 32.53 30.73 34.71 28.98 27.71 Rb 171.1 132.8 124.6 144.6 178.7 207.0 Cs 4.35 0.86 0.66 2.67 2.37 2.87 Sr 69.54 153.75 157.88 26.47 24.55 13.01 Sc 5.70 18.83 18.78 3.17 3.03 1.81 Zr 386 1425 1437 359 346 142

119 Member Messa Falls Tuff HRT B Messa Falls Tuff Messa Falls Tuff Messa Falls Tuff LCT -B

Unit Messa Falls Tuff Member B Messa Falls Tuff Messa Falls Tuff Messa Falls Tuff Member B

along Hwy N of along Hwy N of along Hwy N of along Hwy N of along Hwy N of Locality Ashton Ashton Ashton Ashton Ashton Island Park northing 4891167 4885481 4885503 4885503 4885503 4927904 easting (12) 456941 464691 464687 464687 464687 476522 Lithology pumice tuff pumice pumice pumice tuff Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 1.292 2.053 1.292 1.292 1.292 0.64 Age error 0.005 0.006 0.005 0.005 0.005 0.002 Sample # 08CP49P 08CP50 08CP51 08CP52 08CP53 08CP54 Date 2-Jan-09 2-Jan-09 2-Jan-09 2-Jan-09 3-Jan-09 3-Jan-09 SiO2 79.17 70.34 76.38 74.97 74.34 75.97 TiO2 0.09 0.48 0.19 0.20 0.20 0.18 Al2O3 11.50 14.25 12.92 13.73 14.42 12.87 FeO* 0.88 4.28 1.79 1.94 1.86 1.56 MnO 0.01 0.10 0.04 0.04 0.04 0.02 MgO 0.03 0.22 0.09 0.09 0.09 0.00 CaO 0.38 1.35 0.68 0.76 0.67 0.51 Na2O 3.17 3.99 2.73 2.88 3.06 3.56 K2O 4.74 4.87 5.15 5.36 5.31 5.31 P2O5 0.02 0.11 0.02 0.03 0.03 0.02 Raw 98.14 97.63 96.23 96.63 96.14 98.94 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.00 2.77 1.87 1.86 17.02 0.45 Cr 3.20 3.60 2.90 2.80 2.60 1.30 Sc 2.20 6.70 4.00 3.90 3.20 1.40 V 0.20 13.60 0.80 2.10 2.40 1.90 Ba 26.90 3299.50 390.40 621.00 753.20 597.30 Rb 209.70 103.70 188.30 161.50 145.00 178.50 Sr 4.40 110.30 29.00 41.60 50.00 20.60 Zr 123.50 754.00 258.20 289.00 277.90 343.80 Y 50.50 57.50 85.80 94.80 68.90 54.60 Nb 61.80 39.80 49.30 45.90 41.90 57.30 Ga 20.30 24.50 23.30 23.20 23.20 23.50 Cu 11.30 4.90 2.20 1.70 2.00 1.80 Zn 45.70 133.70 84.50 113.80 77.30 82.40 Pb 36.30 21.90 38.60 42.60 35.30 27.80 La 84.90 73.20 90.80 100.70 90.40 101.10 Ce 101.80 152.20 176.30 187.20 176.10 213.90 Th 38.60 18.00 33.40 34.00 30.70 31.50 Nd 66.40 64.00 68.20 73.50 63.80 72.70 U 7.90 3.00 6.30 5.20 4.10 5.10

ICP-MS (ppm) La 82.97 78.02 95.58 104.43 92.27 105.90 Ce 100.61 156.11 177.02 190.08 180.65 217.55 Pr 20.06 17.13 19.94 21.67 19.02 21.94 Nd 68.73 64.62 70.21 76.16 66.32 75.60 Sm 14.60 13.13 14.42 15.66 13.16 14.13 Eu 0.21 4.48 0.88 1.29 1.42 1.38 Gd 12.46 12.20 14.12 15.33 12.38 11.61 Tb 2.18 1.94 2.42 2.55 2.02 1.97 Dy 12.65 11.59 14.69 15.49 12.03 11.81 Ho 2.41 2.32 3.10 3.20 2.49 2.37 Er 6.22 6.25 8.41 8.76 6.66 6.57 Tm 0.93 0.90 1.23 1.26 0.97 0.96 Yb 5.71 5.55 7.52 7.60 5.93 6.18 Lu 0.80 0.88 1.14 1.17 0.91 0.92 Ba 27 3415 401 637 771 604 Th 37.13 17.71 33.89 32.73 31.07 30.08 Nb 62.56 39.46 50.18 47.22 42.44 58.13 Y 48.77 57.28 86.48 92.85 68.07 53.50 Hf 5.86 18.30 8.91 9.43 9.13 11.28 Ta 4.36 2.46 3.84 3.53 3.39 3.97 U 8.76 3.42 6.26 5.25 4.77 5.63 Pb 37.34 22.47 39.80 43.80 38.41 27.85 Rb 212.5 104.1 192.2 162.3 147.4 179.5 Cs 2.79 1.08 4.72 3.72 3.40 2.56 Sr 4.41 111.75 30.18 41.49 51.68 21.45 Sc 1.46 7.07 3.18 3.42 3.22 2.22 Zr 121 732 256 286 275 340

120 Upper Basin Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek Obsidian Creek Member Member Member Member Member Member Member Gardner River Gardner River Gardner River Gardner River Gardner River Unit Canyon Flow Complex Complex Complex Complex Complex

Locality Canyon Village First Cataract First Cataract First Cataract First Cataract First Cataract northing 4953342 4971113 4971147 4971147 4971147 4971147 easting (12) 540482 521805 522010 522010 522010 522010 Lithology tuff rhyolite rhyolite spheriolite rhyolite basalt Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 4.84 Age error 0.01 Sample # 08CP55 08CP56 08CP57 08CP57B 08CP58 08CP59 Date 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 5-Jan-09 3-Jan-09 SiO2 76.18 76.27 76.94 76.99 76.86 65.00 TiO2 0.33 0.17 0.12 0.12 0.13 0.82 Al2O3 12.65 12.52 12.09 12.39 12.22 14.16 FeO* 1.61 1.82 1.74 1.46 1.60 5.60 MnO 0.02 0.04 0.01 0.03 0.01 0.08 MgO 0.04 0.08 0.02 0.02 0.04 3.02 CaO 0.75 0.60 0.51 0.44 0.55 4.95 Na2O 3.46 3.75 3.70 3.96 3.77 3.40 K2O 4.91 4.71 4.85 4.58 4.79 2.86 P2O5 0.04 0.04 0.02 0.02 0.02 0.10 Raw 98.49 98.23 97.75 98.87 98.92 99.54 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 3.36 3.90 2.03 0.79 0.00 46.88 Cr 3.80 5.80 3.40 1.30 3.60 55.00 Sc 6.80 2.40 1.80 1.80 1.90 13.80 V 4.50 9.00 2.20 1.20 5.70 105.50 Ba 1026.60 519.10 468.00 473.90 493.60 389.20 Rb 165.60 163.80 166.00 165.50 164.60 97.10 Sr 79.00 38.30 25.10 23.20 26.40 205.60 Zr 375.70 228.40 217.30 210.60 216.00 173.40 Y 61.60 44.90 50.90 56.20 54.30 45.00 Nb 49.30 32.70 34.20 34.30 33.80 23.00 Ga 20.40 22.10 21.80 23.00 22.70 21.70 Cu 0.80 3.50 1.90 0.10 2.70 21.30 Zn 87.20 79.40 67.60 74.90 67.50 99.90 Pb 29.90 27.00 23.90 29.00 27.90 16.20 La 76.70 53.30 66.70 73.10 66.70 43.70 Ce 146.70 110.20 115.00 131.30 127.20 84.30 Th 24.80 20.50 20.10 21.20 20.07 11.10 Nd 62.90 42.50 52.40 56.90 50.70 37.00 U 6.80 3.30 3.70 4.90 2.50 3.50

ICP-MS (ppm) La 77.70 53.94 70.02 71.81 70.33 43.69 Ce 150.01 111.28 121.34 132.17 130.62 84.61 Pr 18.26 12.17 15.04 15.88 15.16 9.95 Nd 66.03 44.46 54.96 58.14 55.40 38.08 Sm 13.58 9.65 11.50 12.47 11.60 8.38 Eu 1.99 0.92 0.88 0.90 0.91 1.24 Gd 11.73 8.74 10.54 11.40 10.78 8.32 Tb 1.99 1.56 1.77 1.96 1.85 1.42 Dy 11.82 9.41 10.40 11.63 11.16 8.64 Ho 2.37 1.88 1.99 2.28 2.14 1.71 Er 6.50 5.10 5.26 6.08 5.65 4.47 Tm 0.94 0.74 0.75 0.86 0.82 0.65 Yb 5.75 4.50 4.42 5.20 4.78 3.82 Lu 0.87 0.66 0.66 0.75 0.70 0.57 Ba 1042 526 478 480 492 387 Th 23.99 20.00 19.86 20.57 20.17 11.69 Nb 49.37 33.78 33.72 34.21 32.08 23.29 Y 59.94 43.91 49.47 54.78 54.04 43.62 Hf 10.81 7.95 7.92 7.78 7.88 5.69 Ta 3.44 2.54 2.53 2.56 2.43 1.72 U 6.55 4.21 3.71 4.82 3.70 2.72 Pb 29.84 27.66 24.38 28.88 26.04 17.26 Rb 167.3 166.8 168.9 166.6 165.4 95.8 Cs 4.65 1.96 2.04 3.11 2.05 1.56 Sr 79.44 38.49 24.87 23.42 26.40 204.55 Sc 6.14 2.65 2.00 1.78 1.91 13.19 Zr 372 227 218 209 214 166

121 Junction Butte Junction Butte Sed & Bas of the Sed & Bas of the Member Swan Lake Basalt pC Basalt Basalt Narrows Narrows Overhanging Cliff Overhanging Cliff upper basalt of upper basalt of Unit Swan Lake Basalt Granitic Gniess flow flow the narrows the narrows

west of Calcite Locality Sheepeater's Cliff Lamar Canyon Overhanging Cliff Overhanging Cliff along road Springs overlook northing 4971039 4973680 4971451 4971508 4971726 4972142 easting (12) 521717 556305 548473 548287 548215 547889 Lithology basalt granite basalt basalt basalt basalt Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 0.32 2785 2.16 2.16 1.3 1.3 Age error 0.32 166 0.04 0.04 0.35 0.35 Sample # 08CP60 08CP61 08CP62 08CP63 08CP64 08CP65 Date 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 SiO2 50.50 65.66 56.70 56.18 50.89 56.19 TiO2 1.85 0.86 1.72 1.79 2.16 1.87 Al2O3 15.65 15.84 15.48 15.47 17.93 15.52 FeO* 10.13 5.05 9.50 9.55 12.34 9.74 MnO 0.16 0.07 0.18 0.18 0.15 0.17 MgO 7.34 1.52 3.78 3.96 2.39 3.93 CaO 11.02 3.98 7.23 7.58 8.56 7.43 Na2O 2.65 3.98 3.15 3.10 3.85 3.00 K2O 0.47 2.76 1.85 1.78 1.31 1.73 P2O5 0.23 0.28 0.42 0.42 0.42 0.42 Raw 99.82 98.35 98.01 98.86 95.95 98.38 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 84.72 3.15 23.40 25.90 38.20 23.19 Cr 269.70 11.10 17.30 18.80 17.90 17.10 Sc 30.10 13.10 22.40 24.10 23.30 24.80 V 247.50 75.10 166.90 184.60 251.80 196.20 Ba 179.30 1883.20 781.90 746.40 539.60 740.60 Rb 8.80 99.50 49.00 46.40 21.90 46.70 Sr 346.90 437.00 378.20 379.00 637.60 381.60 Zr 122.80 300.10 270.50 253.50 178.60 246.30 Y 23.90 16.90 32.00 30.90 22.90 33.70 Nb 12.80 8.60 20.70 21.10 35.60 21.60 Ga 17.80 19.20 21.10 19.80 19.10 21.00 Cu 56.90 8.90 20.90 22.90 15.70 20.70 Zn 101.20 69.30 107.70 107.20 124.10 114.30 Pb 1.80 14.10 8.30 8.20 4.10 8.10 La 12.70 37.00 33.60 31.80 30.20 35.30 Ce 31.90 89.10 72.30 68.30 65.80 74.50 Th 3.10 9.90 5.50 5.80 3.10 5.00 Nd 18.40 37.30 37.30 35.70 31.30 36.70 U 0.00 4.10 0.20 0.50 0.50 1.90

ICP-MS (ppm) La 14.38 39.04 37.29 36.49 35.02 37.30 Ce 31.41 86.69 74.50 72.80 68.29 74.46 Pr 4.27 10.25 9.10 8.92 8.24 9.12 Nd 18.76 38.32 36.60 35.99 32.01 37.23 Sm 4.84 6.99 7.72 7.68 6.29 7.99 Eu 1.74 2.02 2.65 2.61 2.13 2.67 Gd 5.20 5.55 7.44 7.26 5.71 7.67 Tb 0.86 0.70 1.14 1.14 0.86 1.20 Dy 5.10 3.78 6.73 6.70 4.95 7.00 Ho 1.01 0.70 1.30 1.30 0.95 1.35 Er 2.55 1.79 3.38 3.30 2.39 3.57 Tm 0.35 0.25 0.47 0.46 0.33 0.49 Yb 2.01 1.54 2.79 2.76 1.97 2.88 Lu 0.30 0.25 0.43 0.42 0.30 0.46 Ba 174 1907 775 741 535 734 Th 1.13 10.55 4.99 4.79 3.07 4.72 Nb 13.22 9.15 21.36 21.33 37.87 21.34 Y 24.66 17.71 32.20 32.02 23.45 34.53 Hf 3.08 7.11 6.55 6.15 4.43 5.99 Ta 0.83 0.73 1.39 1.37 2.31 1.40 U 0.30 3.42 1.10 1.06 0.66 1.02 Pb 1.76 15.12 9.28 8.85 3.91 8.70 Rb 8.7 99.1 49.4 46.5 22.0 46.6 Cs 0.41 2.21 3.53 0.88 0.57 3.76 Sr 352.96 438.71 386.01 387.31 661.01 387.60 Sc 30.66 13.88 23.04 24.13 23.95 24.41 Zr 115 282 261 243 171 236

122 Undine Falls Member Basalt Swan Lake Basalt Roaring Mountain Roaring Mountain Roaring Mountain LCT-B Undine Falls, Crystal Spring Crystal Spring Crystal Spring Unit upper flow Swan Lake Basalt flow flow flow member B

blacktail plateau E of Apollinaris E of Apollinaris E of Apollinaris E of Apollinaris E of Apollinaris Locality rd Spring Spring Spring Spring Spring northing 4978228 4965761 4965942 4965942 4965991 4965579 easting (12) 536186 521849 522575 522575 522584 521206 Lithology basalt basalt obsidian obsidian pumice tuff Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 0.6 0.32 0.08 0.08 0.08 0.64 Age error 0.1 0.32 0.002 0.002 0.002 0.002 Sample # 08CP66 08CP67 08CP68 08CP69 08CP70 08CP71 Date 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 3-Jan-09 SiO2 49.46 50.57 76.58 75.87 76.06 77.26 TiO2 1.83 1.66 0.12 0.16 0.15 0.11 Al2O3 16.51 15.87 12.34 12.43 12.48 12.19 FeO* 11.47 10.25 1.37 1.64 1.59 1.40 MnO 0.17 0.16 0.03 0.03 0.03 0.02 MgO 6.97 7.55 0.22 0.43 0.36 0.02 CaO 9.87 10.57 0.71 0.99 0.83 0.39 Na2O 2.95 2.69 3.76 3.67 3.71 3.55 K2O 0.53 0.47 4.85 4.75 4.77 5.02 P2O5 0.24 0.20 0.01 0.02 0.02 0.02 Raw 100.61 99.86 98.29 98.82 99.14 98.72 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 83.24 94.98 0.22 3.96 4.00 0.55 Cr 56.20 130.80 5.10 7.60 7.50 3.80 Sc 27.60 29.70 2.40 3.30 3.30 1.80 V 244.60 224.80 6.70 13.80 12.30 0.00 Ba 235.50 205.10 38.80 46.50 45.50 92.70 Rb 7.70 8.00 229.60 228.20 224.30 226.60 Sr 416.50 378.20 11.30 22.10 18.60 7.10 Zr 127.30 114.60 159.30 159.20 160.70 188.60 Y 24.50 23.10 76.30 75.50 63.60 40.30 Nb 11.50 10.10 41.20 40.60 41.20 62.90 Ga 21.20 17.70 22.90 22.90 24.00 23.80 Cu 30.80 43.70 1.50 3.90 5.10 0.30 Zn 113.60 98.10 73.80 85.00 71.30 67.30 Pb 2.80 3.40 34.70 41.20 32.30 27.60 La 15.90 12.80 60.90 57.10 58.80 56.80 Ce 36.70 31.60 116.10 116.50 110.30 116.30 Th 2.70 2.00 30.10 29.00 29.20 30.90 Nd 20.20 18.90 48.30 49.80 43.30 38.10 U 1.00 0.70 5.90 8.10 7.40 6.40

ICP-MS (ppm) La 15.23 12.84 60.88 59.69 55.27 58.52 Ce 33.05 28.02 121.49 118.90 113.47 114.10 Pr 4.46 3.80 14.00 13.81 12.35 11.29 Nd 19.64 16.85 51.85 50.96 45.04 37.82 Sm 5.01 4.29 12.33 12.20 10.70 7.97 Eu 1.79 1.60 0.20 0.25 0.23 0.35 Gd 5.17 4.75 12.47 12.34 10.68 7.22 Tb 0.86 0.78 2.28 2.26 1.97 1.37 Dy 5.08 4.69 14.24 14.07 12.30 8.81 Ho 1.01 0.92 2.87 2.82 2.44 1.80 Er 2.52 2.32 7.71 7.54 6.59 4.97 Tm 0.36 0.32 1.13 1.11 0.98 0.76 Yb 2.10 1.85 6.66 6.56 5.96 4.83 Lu 0.32 0.28 0.98 0.96 0.87 0.73 Ba 233 199 39 47 47 93 Th 1.17 1.30 29.16 28.58 29.03 31.00 Nb 12.05 10.33 41.70 39.97 41.11 62.69 Y 24.83 22.56 76.94 74.73 62.20 39.49 Hf 3.29 2.94 7.68 7.61 7.68 8.03 Ta 0.77 0.66 3.22 3.16 3.26 4.73 U 0.33 0.32 6.91 6.77 6.78 7.65 Pb 2.45 2.63 34.73 41.50 32.04 27.86 Rb 8.6 8.4 237.4 231.4 225.8 227.6 Cs 0.19 0.15 5.04 4.86 4.41 2.17 Sr 422.57 385.12 12.15 22.65 18.95 7.57 Sc 27.71 28.54 2.20 2.92 2.76 1.75 Zr 119 107 162 160 161 188

123 Member Central Plateau Central Plateau HRT-C HRT-B HRT-A HRT-A

Unit Tuff of Bluff Point Tuff of Bluff Point Member C Member B Member A Member A

Locality roadcut roadcut S of YNP S of YNP S of YNP S of YNP northing 4922359 4922359 4879068 4878960 4879222 4878960 easting (12) 534806 534806 524716 524690 524847 524690 Lithology wx glass tuff tuff tuff tuff tuff Source CJP08 CJP08 CJP08 CJP08 CJP08 CJP08 Age (Ma) 0.11 0.11 2.053 2.053 2.053 2.053 Age error 0.1 0.1 0.006 0.006 0.006 0.006 Sample # 08CP73 08CP74 08CP75 08CP76 08CP77 08CP78 Date 3-Jan-09 3-Jan-09 4-Jan-09 4-Jan-09 4-Jan-09 4-Jan-09 SiO2 77.47 77.23 77.26 75.85 76.85 77.01 TiO2 0.17 0.17 0.20 0.16 0.23 0.23 Al2O3 11.95 12.10 11.81 12.67 11.80 11.80 FeO* 1.35 1.36 2.16 1.83 2.54 2.49 MnO 0.03 0.03 0.02 0.11 0.05 0.04 MgO 0.04 0.04 0.00 0.04 0.04 0.00 CaO 0.40 0.48 0.42 0.56 0.53 0.47 Na2O 3.39 3.21 3.48 3.57 3.44 3.51 K2O 5.20 5.36 4.63 5.19 4.49 4.42 P2O5 0.01 0.01 0.02 0.02 0.03 0.03 Raw 98.60 96.48 98.47 98.29 98.19 97.57 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 0.00 0.42 0.18 0.00 0.16 0.00 Cr 2.60 2.50 3.20 3.10 3.10 3.80 Sc 1.80 2.40 2.70 2.70 4.60 4.30 V 0.90 1.60 2.30 0.50 3.10 2.10 Ba 376.90 431.30 1931.90 1079.60 2050.20 2042.50 Rb 180.10 180.80 140.10 163.80 130.70 129.90 Sr 15.30 18.40 96.80 35.10 125.20 133.80 Zr 230.90 227.80 381.50 288.00 428.70 445.70 Y 55.10 60.80 31.40 70.30 47.20 39.70 Nb 47.00 46.60 26.60 46.80 26.60 26.50 Ga 18.00 19.80 19.60 23.20 20.40 20.50 Cu 0.20 0.40 5.60 4.50 5.40 3.20 Zn 60.40 51.30 93.90 98.20 113.20 101.40 Pb 30.00 18.20 36.20 24.40 35.60 35.70 La 83.50 83.90 51.70 137.80 64.10 46.80 Ce 165.70 163.70 88.20 327.40 118.20 100.00 Th 26.50 26.90 19.00 28.30 18.30 18.10 Nd 61.90 60.90 40.10 100.60 47.90 40.90 U 7.60 5.30 4.70 6.40 4.60 3.80

ICP-MS (ppm) La 85.21 86.73 54.24 140.87 61.92 51.34 Ce 163.99 164.78 90.05 335.90 121.23 100.48 Pr 17.80 18.10 11.95 29.08 13.81 11.39 Nd 62.77 63.96 43.40 104.08 50.99 42.07 Sm 12.22 12.69 8.46 19.31 10.61 9.03 Eu 0.88 0.90 2.85 1.72 3.29 3.33 Gd 10.80 11.20 7.07 15.90 9.67 8.23 Tb 1.89 1.93 1.12 2.59 1.60 1.37 Dy 11.63 11.92 6.47 15.31 9.66 8.12 Ho 2.29 2.37 1.26 2.95 1.92 1.61 Er 6.18 6.45 3.38 7.98 5.14 4.24 Tm 0.92 0.96 0.49 1.18 0.74 0.63 Yb 5.60 5.88 2.99 7.28 4.46 3.74 Lu 0.84 0.87 0.46 1.09 0.70 0.58 Ba 377 445 1988 1104 2125 2126 Th 26.44 26.20 18.41 27.60 17.68 17.44 Nb 46.62 46.36 26.83 47.84 27.08 27.23 Y 54.99 61.54 30.66 69.66 46.93 40.13 Hf 8.33 8.37 10.34 9.83 11.11 11.39 Ta 3.38 3.36 1.93 3.30 1.90 1.88 U 7.00 6.06 4.56 4.98 4.17 3.69 Pb 29.71 19.02 37.23 24.75 35.28 35.93 Rb 181.5 183.6 141.8 164.7 132.6 131.6 Cs 3.61 4.41 2.94 2.12 2.41 2.70 Sr 15.88 19.20 97.82 36.17 125.70 135.83 Sc 2.40 2.30 3.12 2.25 4.28 3.94 Zr 232 230 377 289 426 450

124 Basalt of Geode Member Central Plateau Ck pC Obsidian Creek Obsidian Creek Obsidian Creek Basalt of Geode Unit Aster Creek Flow Creek Granitic Gniess Grizzly Lake Grizzly Lake Grizzly Lake

Chief Joseph Senic North portion of North portion of enlcave in Grizzly Locality just off the road north outcrop Hwy Grizzly Lake Flow Grizzly Lake Flow Lake Flow northing 4903645 4978733 4973680 4965601 4965278 4963487 easting (12) 529830 540295 556305 519477 519397 519106 Lithology vitric tuff basalt granite rhyolite rhyolite basalt Source CJP08 CJP08 CJP08 CJP09 CJP09 CJP09 Age (Ma) 0.11 0.3 2785 0.2633 0.2633 0.2633 Age error 0.1 0.3 166 0.0034 0.0034 0.0034 Sample # 08CP79 08CP80 08CP81 GL46 GL47 GL51 Date 4-Jan-09 4-Jan-09 4-Jan-09 5-Sep-09 5-Sep-09 5-Sep-09 SiO2 77.23 53.94 73.04 77.74 77.91 57.14 TiO2 0.17 1.69 0.20 0.11 0.11 1.31 Al2O3 12.19 15.71 15.14 11.91 11.92 14.96 FeO* 1.41 10.10 1.56 1.31 1.32 8.28 MnO 0.05 0.15 0.01 0.08 0.04 0.16 MgO 0.04 5.57 0.38 0.05 0.04 5.63 CaO 0.36 8.32 1.87 0.40 0.35 7.84 Na2O 3.30 2.86 4.63 3.46 3.39 2.91 K2O 5.23 1.44 3.14 4.92 4.91 1.59 P2O5 0.02 0.21 0.04 0.01 0.01 0.18 Raw 97.87 99.43 99.09 96.93 97.10 99.52 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 1.02 72.14 0.00 3.10 0.90 65.60 Cr 3.30 47.40 5.60 2.90 3.60 64.60 Sc 3.80 24.80 3.00 2.40 1.90 22.20 V 1.30 211.10 15.20 3.00 1.00 156.10 Ba 362.00 499.70 1008.80 98.00 114.00 197.80 Rb 180.30 38.30 61.60 210.10 201.30 49.20 Sr 17.90 310.90 308.00 7.40 8.50 277.70 Zr 231.00 191.30 132.20 174.00 174.90 143.10 Y 42.10 31.50 4.20 43.00 31.60 35.10 Nb 48.00 12.90 1.90 57.60 55.00 19.10 Ga 20.80 19.40 20.10 22.30 22.60 20.70 Cu 0.00 36.60 0.10 2.30 1.70 39.50 Zn 61.50 106.20 34.60 58.00 47.70 98.30 Pb 27.70 7.00 28.10 26.40 26.00 9.20 La 74.50 32.20 41.90 51.60 38.60 25.50 Ce 134.70 58.50 70.70 135.30 142.60 58.20 Th 26.90 4.50 28.00 28.90 28.10 7.80 Nd 51.40 27.90 22.80 32.40 23.40 27.70 U 5.50 1.60 1.40 7.10 6.50 2.10

ICP-MS (ppm) La 75.95 28.71 40.45 51.28 43.56 27.97 Ce 138.03 58.93 66.88 140.12 147.12 57.20 Pr 15.77 7.33 6.63 10.12 7.44 6.94 Nd 53.99 29.28 21.48 34.12 24.85 27.50 Sm 10.56 6.76 3.37 7.70 5.31 6.59 Eu 0.83 1.95 0.71 0.33 0.39 1.41 Gd 8.52 6.71 2.07 7.00 5.05 6.50 Tb 1.45 1.10 0.23 1.36 1.01 1.12 Dy 8.61 6.48 0.94 8.91 6.73 6.80 Ho 1.74 1.29 0.15 1.82 1.42 1.34 Er 4.81 3.29 0.33 5.23 4.19 3.52 Tm 0.72 0.47 0.04 0.80 0.67 0.49 Yb 4.48 2.84 0.24 5.26 4.36 2.91 Lu 0.68 0.44 0.04 0.77 0.65 0.43 Ba 373 495 1020 101 115 192 Th 26.73 5.13 27.24 28.39 28.06 6.65 Nb 48.78 13.55 2.49 58.63 55.77 18.11 Y 42.26 32.00 3.64 41.69 30.48 33.75 Hf 8.35 5.09 3.88 7.35 7.27 4.36 Ta 3.62 0.91 0.12 4.33 4.09 1.27 U 6.05 0.73 1.23 7.01 6.55 1.49 Pb 27.69 7.89 28.17 26.11 25.73 8.91 Rb 184.6 39.6 62.9 210.7 205.6 47.1 Cs 3.52 0.51 0.50 2.20 3.05 0.75 Sr 18.36 318.52 310.59 9 9 272 Sc 2.46 24.57 2.43 2.8 2.5 22.0 Zr 235 183 131 178 179 143

125 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Dunraven Road Dunraven Road Unit Flow Canyon Flow Canyon Flow Canyon Flow Flow Canyon Flow?

West portion top small ridge in ring top of canyon? Locality of ring fracture fracture DRF? Canyon Flow on southern hill - Canyon Flow? northing 4955406 4955210 4954402 4954397 4954729 4955445 easting (12) 541714 541831 542025 542341 542576 542567 Lithology wx glass tuff glassy altered vitrophyre glass Source CJP09 CJP09 CJP09 CJP09 CJP09 CJP09 Age (Ma) 0.486 0.484 0.484 0.484 0.486 0.484 Age error 0.042 0.015 0.015 0.015 0.042 0.015 Sample # 0908 0911 0915 0917 0919 0920 Date 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 SiO2 77.24 75.75 76.43 76.63 77.50 74.75 TiO2 0.12 0.34 0.28 0.23 0.12 0.40 Al2O3 12.28 12.61 12.52 12.50 12.01 12.82 FeO* 1.17 1.93 1.52 1.40 1.17 2.43 MnO 0.03 0.05 0.03 0.03 0.03 0.09 MgO 0.05 0.08 0.09 0.06 0.04 0.25 CaO 0.49 0.83 0.67 0.60 0.50 1.17 Na2O 3.47 3.52 3.51 3.46 3.47 3.40 K2O 5.12 4.83 4.90 5.06 5.15 4.63 P2O5 0.02 0.05 0.03 0.03 0.01 0.05 Raw 97.91 97.79 97.66 97.55 97.84 96.15 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 3.60 1.90 2.30 3.00 2.00 4.30 Cr 3.30 4.10 3.30 4.10 3.00 3.50 Sc 4.20 6.00 4.20 5.70 4.50 5.90 V 2.80 2.00 4.00 3.90 1.50 7.00 Ba 655.40 1031.40 928.60 866.30 642.50 1106.70 Rb 169.70 164.10 167.10 168.80 166.40 158.60 Sr 20.40 86.00 62.60 54.70 17.50 106.20 Zr 194.20 378.10 326.40 285.80 190.60 431.00 Y 52.70 62.90 64.80 57.80 53.20 62.30 Nb 33.00 48.30 46.40 42.10 34.10 45.30 Ga 19.60 20.60 20.60 20.10 19.80 20.80 Cu 0.00 2.00 0.10 1.80 0.30 3.20 Zn 47.90 74.30 50.50 49.60 50.00 88.30 Pb 32.40 31.50 29.90 32.00 30.80 30.20 La 62.40 83.60 79.00 76.70 60.00 72.90 Ce 118.10 144.00 146.20 153.30 116.60 141.00 Th 21.00 22.70 23.60 22.50 20.40 22.60 Nd 50.10 63.20 61.40 59.70 45.80 58.00 U 5.60 6.40 6.40 5.10 3.70 6.30

ICP-MS (ppm) La 65.64 81.83 81.14 79.47 62.98 76.51 Ce 125.69 147.35 149.60 158.19 119.96 147.86 Pr 14.21 17.95 17.75 17.39 13.51 16.59 Nd 51.21 65.62 64.62 62.50 48.76 61.19 Sm 10.67 13.43 13.05 12.71 10.18 12.61 Eu 0.74 2.12 1.67 1.50 0.72 2.32 Gd 9.61 12.20 11.75 11.42 9.35 11.57 Tb 1.65 2.08 2.01 1.93 1.61 1.96 Dy 9.89 12.37 12.24 11.62 9.89 11.82 Ho 1.95 2.47 2.40 2.25 1.97 2.39 Er 5.23 6.50 6.53 6.04 5.34 6.47 Tm 0.76 0.96 0.95 0.87 0.77 0.95 Yb 4.67 5.93 5.79 5.38 4.80 5.87 Lu 0.69 0.90 0.87 0.80 0.73 0.89 Ba 677 1062 947 902 666 1147 Th 20.81 23.04 23.39 22.34 20.34 21.52 Nb 33.62 48.09 46.75 42.94 33.83 46.31 Y 50.58 60.58 62.45 55.56 51.24 60.86 Hf 7.08 10.77 9.67 9.14 6.91 11.73 Ta 2.48 3.34 3.23 3.02 2.46 3.16 U 4.57 5.76 5.83 5.41 4.54 5.32 Pb 31.94 30.05 29.51 30.81 31.44 30.05 Rb 170.1 164.2 167.5 170.7 167.4 157.1 Cs 3.44 3.18 3.13 2.63 3.40 3.39 Sr 21 86 63 55 18 106 Sc 4.7 6.3 5.3 5.9 4.7 7.3 Zr 201 384 332 296 197 435

126 Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Dunraven Road Tuff of Uncle Unit Flow Tom's Trail Canyon Flow Canyon Flow? Canyon Flow? Canyon Flow?

stoney interior Brink of Lower just off of 7-mile flow top breccia? flow top breccia? Locality from ring fracture Falls hole trail Near DRF Near DRF near DRF northing 4955642 4951699 4954608 4955155 4955140 4955346 easting (12) 542334 539686 543767 543124 542797 543014 Lithology tuff ignimbrite wx tuff breccia breccia wx tuff Source CJP09 CJP09 CJP09 CJP09 CJP09 CJP09 Age (Ma) 0.486 0.481 0.484 0.484 0.484 0.484 Age error 0.042 0.0? 0.015 0.015 0.015 0.015 Sample # 0921 0922 0923 0925 0926 0927 Date 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 SiO2 77.57 84.12 75.99 80.83 75.62 77.27 TiO2 0.12 0.17 0.34 0.23 0.37 0.27 Al2O3 12.10 8.68 12.51 10.61 12.80 12.92 FeO* 1.22 0.97 2.16 1.20 2.25 1.82 MnO 0.01 0.02 0.02 0.04 0.05 0.02 MgO 0.01 0.09 0.08 0.05 0.08 0.01 CaO 0.37 0.54 0.65 0.55 0.95 0.28 Na2O 3.44 1.55 3.28 2.30 2.76 2.56 K2O 5.15 3.82 4.93 4.17 5.08 4.83 P2O5 0.01 0.02 0.04 0.02 0.05 0.03 Raw 97.55 92.76 96.63 94.43 94.43 93.89 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 3.00 2.80 2.00 3.10 2.40 0.80 Cr 2.80 6.70 2.80 2.90 3.40 2.30 Sc 3.40 3.00 6.00 4.30 5.80 3.60 V 1.40 5.30 4.10 0.40 6.10 4.10 Ba 656.50 514.30 972.30 693.90 1035.90 882.60 Rb 163.90 144.60 171.10 136.20 168.20 132.50 Sr 18.00 46.00 70.30 46.30 86.70 48.00 Zr 190.00 232.80 379.60 256.10 398.20 299.50 Y 28.20 45.20 68.30 53.00 65.20 35.20 Nb 33.30 31.50 48.40 39.80 47.00 48.60 Ga 19.60 13.40 20.00 17.20 19.50 18.90 Cu 2.00 0.80 1.30 2.00 0.80 1.20 Zn 45.60 42.40 63.60 49.20 68.60 31.10 Pb 30.00 21.40 26.30 27.60 30.00 25.70 La 35.70 53.40 81.80 61.50 75.10 48.40 Ce 68.50 102.30 156.40 127.30 147.40 100.90 Th 19.90 17.10 23.60 21.50 23.20 22.50 Nd 25.10 39.40 63.90 51.10 60.00 33.00 U 4.70 6.90 4.90 5.80 5.70 5.20

ICP-MS (ppm) La 37.26 57.21 82.72 66.49 77.57 53.90 Ce 72.50 107.93 157.54 128.84 149.71 102.43 Pr 7.66 12.16 18.46 14.50 17.07 9.89 Nd 26.93 43.16 67.15 52.17 62.25 34.42 Sm 5.72 8.55 13.83 10.61 12.86 6.91 Eu 0.69 0.89 1.89 1.23 2.04 1.06 Gd 5.11 7.80 12.91 9.60 11.90 6.24 Tb 0.93 1.34 2.18 1.63 2.02 1.11 Dy 5.70 8.14 13.22 10.00 12.22 6.79 Ho 1.16 1.65 2.61 2.01 2.48 1.39 Er 3.21 4.49 7.04 5.38 6.73 3.81 Tm 0.49 0.66 1.01 0.80 0.99 0.56 Yb 3.11 4.12 6.26 4.93 6.09 3.45 Lu 0.46 0.63 0.93 0.75 0.93 0.52 Ba 656 536 1001 719 1066 914 Th 20.39 17.34 23.72 21.16 22.94 22.78 Nb 33.75 32.71 48.70 40.68 47.58 48.50 Y 27.03 43.44 66.49 51.23 64.03 33.53 Hf 6.79 7.29 10.63 7.95 11.26 9.09 Ta 2.50 2.35 3.44 2.95 3.31 3.48 U 4.35 6.26 5.33 5.11 5.70 5.01 Pb 28.49 21.50 26.91 27.08 30.84 24.90 Rb 167.3 153.9 175.0 140.7 171.2 134.4 Cs 1.84 12.12 3.80 12.85 5.01 1.39 Sr 20 48 72 47 88 49 Sc 3.9 3.2 5.9 4.5 6.9 4.1 Zr 195 242 373 266 403 302

127 Member Ts Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Canyon Flow - Canyon Flow - Canyon Flow - Canyon Flow - Canyon Flow - Unit Absaroka basal basal upper upper middle

near DRF along Locality road Wapiti Lake Trail Wapiti Lake Trail Wapiti Lake Trail Wapiti Lake Trail Wapiti Lake Trail northing 4956221 4949539 4949551 4949631 4949631 4949650 easting (12) 541684 555886 555907 555899 555899 555943 Lithology vol. sediment vitric vitric breccia vitric-tuff tuff Source CJP09 CJP09 CJP09 CJP09 CJP09 CJP09 Age (Ma) 55 0.484 0.484 0.484 0.484 0.484 Age error 1 0.015 0.015 0.015 0.015 0.015 Sample # 0931 0933 0934 0935A 0935B 0936 Date 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 6-Sep-09 SiO2 69.70 74.57 75.01 73.98 76.07 75.74 TiO2 0.43 0.39 0.36 0.45 0.34 0.35 Al2O3 15.65 13.33 12.88 13.97 12.73 12.87 FeO* 3.27 2.02 2.11 1.68 1.41 1.55 MnO 0.05 0.06 0.06 0.05 0.05 0.07 MgO 1.37 0.24 0.23 0.28 0.14 0.14 CaO 2.47 1.29 1.15 1.54 0.89 0.94 Na2O 3.95 3.57 3.49 3.80 3.55 3.56 K2O 2.96 4.47 4.68 4.20 4.80 4.74 P2O5 0.15 0.06 0.05 0.07 0.04 0.04 Raw 95.42 94.83 95.78 97.50 97.33 97.60 Total 100.00 100.00 100.00 100.00 100.00 100.00

(ppm) Ni 22.70 1.80 4.40 3.20 2.10 0.70 Cr 51.10 4.90 4.40 10.00 3.10 5.60 Sc 6.70 6.40 6.00 8.40 5.20 6.10 V 55.60 6.90 5.50 13.20 6.20 5.50 Ba 1705.50 1191.20 1076.50 1360.40 1058.10 1119.10 Rb 67.70 143.80 153.80 123.90 159.70 157.30 Sr 490.10 125.10 100.00 173.00 87.20 102.40 Zr 167.10 409.90 377.30 441.10 384.60 378.40 Y 11.80 61.10 62.20 45.20 57.00 59.20 Nb 5.40 43.70 46.20 41.90 47.80 46.70 Ga 17.00 19.90 20.40 22.60 21.20 20.10 Cu 12.20 1.80 1.20 4.00 1.00 1.40 Zn 43.30 72.40 75.30 60.90 60.30 73.10 Pb 20.30 28.50 29.90 27.80 31.10 31.60 La 33.80 74.00 75.10 65.10 76.50 72.70 Ce 59.20 142.90 143.60 128.80 142.60 143.50 Th 7.40 21.20 22.00 19.30 23.40 22.10 Nd 21.90 56.00 59.50 48.90 55.20 58.40 U 1.10 4.90 4.70 5.20 7.20 5.80

ICP-MS (ppm) La 35.31 75.60 75.40 66.04 76.27 75.70 Ce 59.50 145.65 144.60 130.94 144.96 148.46 Pr 6.32 16.38 16.41 13.96 16.41 16.52 Nd 21.88 59.50 59.78 50.26 58.83 60.19 Sm 3.66 12.18 12.25 10.02 11.88 12.36 Eu 1.01 2.56 2.22 2.90 2.04 2.22 Gd 2.84 11.39 11.15 8.76 10.66 11.19 Tb 0.40 1.91 1.92 1.45 1.83 1.91 Dy 2.18 11.58 11.76 8.75 11.06 11.61 Ho 0.41 2.34 2.35 1.73 2.24 2.30 Er 1.08 6.30 6.45 4.72 6.09 6.27 Tm 0.15 0.92 0.93 0.70 0.89 0.91 Yb 0.92 5.66 5.78 4.41 5.58 5.70 Lu 0.15 0.86 0.89 0.68 0.84 0.86 Ba 1753 1237 1106 1394 1080 1144 Th 7.10 21.09 22.08 18.96 23.38 22.44 Nb 4.85 44.94 46.76 41.94 48.04 46.50 Y 10.68 59.49 60.72 43.80 54.58 56.83 Hf 4.39 11.44 10.68 11.72 11.04 10.90 Ta 0.34 3.11 3.25 2.80 3.39 3.27 U 1.20 5.34 5.40 4.75 5.87 5.59 Pb 19.10 28.45 29.06 26.82 30.92 30.39 Rb 67.9 147.8 156.2 123.8 159.7 158.9 Cs 2.71 3.81 3.78 3.08 3.66 3.19 Sr 493 126 101 168 87 102 Sc 6.7 7.3 7.2 8.6 6.2 6.7 Zr 170 427 389 447 394 389

128 Member Upper Basin Upper Basin Upper Basin Upper Basin Canyon Flow - Tuff of Sulphur Tuff of Sulphur Unit middle Creek Creek Canyon Flow

Locality Wapiti Lake Trail Wapiti Lake Trail Wapiti Lake Trail Wapiti Lake Trail northing 4949632 4949636 4949629 4949775 easting (12) 555944 555963 555977 556089 Lithology tuff vitric tuff tuff Source CJP09 CJP09 CJP09 CJP09 Age (Ma) 0.484 0.484 0.479 0.479 Age error 0.015 0.015 0.01 0.01 Sample # 0937 0938 0939 0940 Date 6-Sep-09 6-Sep-09 6-Sep-09 9/6/2010 SiO2 75.40 75.17 76.01 76.03 TiO2 0.37 0.38 0.36 0.34 Al2O3 12.86 12.99 12.73 12.46 FeO* 1.83 2.14 1.55 1.75 MnO 0.05 0.05 0.05 0.04 MgO 0.13 0.14 0.11 0.13 CaO 1.00 0.96 0.82 0.87 Na2O 3.64 3.51 3.49 3.44 K2O 4.67 4.63 4.84 4.91 P2O5 0.05 0.03 0.04 0.03 Raw 97.87 97.60 97.96 97.11 Total 100.00 100.00 100.00 100.00

(ppm) Ni 1.70 2.40 1.60 2.10 Cr 4.50 5.50 4.40 4.30 Sc 6.00 6.50 8.40 6.30 V 3.50 8.00 5.10 4.70 Ba 1141.90 1102.20 1068.20 1029.10 Rb 152.40 153.20 166.80 167.90 Sr 105.40 101.00 90.90 81.10 Zr 404.10 406.80 400.60 384.00 Y 74.30 76.80 55.50 58.00 Nb 46.60 46.90 47.90 48.30 Ga 21.50 20.50 19.90 19.70 Cu 1.60 1.90 2.00 1.70 Zn 92.90 71.60 57.20 55.10 Pb 30.50 29.60 31.30 29.50 La 80.00 77.30 76.10 74.40 Ce 157.60 145.80 146.70 142.80 Th 21.90 22.70 23.90 24.20 Nd 66.60 64.90 57.40 58.20 U 4.80 7.00 5.30 5.90

ICP-MS (ppm) La 83.77 80.74 78.09 76.52 Ce 160.70 155.12 152.19 145.76 Pr 18.81 18.37 17.07 16.34 Nd 70.46 68.58 61.82 59.15 Sm 14.73 14.70 12.52 12.07 Eu 2.48 2.39 2.10 1.94 Gd 13.91 14.18 11.33 10.84 Tb 2.37 2.46 1.92 1.87 Dy 14.33 14.94 11.59 11.40 Ho 2.91 3.01 2.29 2.28 Er 7.94 8.04 6.19 6.21 Tm 1.14 1.17 0.90 0.91 Yb 7.10 7.17 5.54 5.65 Lu 1.09 1.10 0.84 0.86 Ba 1181 1138 1101 1056 Th 22.17 22.44 23.27 23.80 Nb 46.95 47.53 48.72 49.22 Y 71.36 74.15 53.48 56.14 Hf 11.51 11.51 11.34 10.98 Ta 3.24 3.28 3.39 3.44 U 5.57 5.85 5.88 5.88 Pb 29.46 30.49 38.68 29.28 Rb 154.5 153.5 166.2 167.4 Cs 3.10 3.63 3.57 3.18 Sr 105 100 90 80 Sc 6.9 7.1 8.5 6.8 Zr 417 418 410 397

129

APPENDIX B

RESULTS FROM EC-RAXFC MODELS

EC-RAXFC Results - Melts Page MODEL A

Equilibration Parameters tlm 1184 degC 18O/16O in magma 5.8 Magma a 450 Mro 0.5 Element Name Sr Nd Pb Teq Norm 0.80 tmo 1184 degC 18O/16O in assimilant 0.5 Magma b -11 Episodic Recharge Magma: conc. 312 23 15 Teq deg C 894.03 tla 1129 degC 18O/16O in recharge 5.8 Assimilant a 400 Episode deltaMri Tm,i mr,i d,i bulk Dmo 4 0.4 0.5 Mm 0.41 tao 450 degC Oxygen conc magma 0.47 Assimilant b -11 1 0.2 1000 0.3 2 enthalpy 0 0 0 Mao 2.09 tlr 1184 degC Oxygen conc assimilant 0.5 Recharge Magma a 450 2 0.2 1175 0.3 2 Assimilant: conc. 436 38 15 Ma* 0.29 tro 1184 degC Oxygen conc recharge 0.47 Recharge Magma b -11 3 0.1 1155 0.3 2 bulk Dao 6 0.6 0.7 Mc 1.29 ts 750 degC enthalpy 0 0 0 Men 0.10 cpm 1100 J/kg K Recharge: conc. 300 23 15 Ms 1.38 cpa 1000 J/kg K bulk Dro 4 0.4 0.5 fa 0.14 cpr 1100 J/kg K enthalpy 0 0 0 fm 0.08 hm 400000 J/kg Isotope Name 87Sr/86Sr 143Nd/144Nd 206Pb/204Pb fr 0.08 ha 350000 J/kg ratio in magma 0.706451 0.512385 17 hr 400000 J/kg ratio in assimilant 0.728666 0.510803 21.9 X 1 Normalized fraction of Wallrock melt ratio in recharge 0.706451 0.512385 17 mixed into Magma body

Norm T T magma Norm T T assim magma (deg C) assim (deg C) Mm fa Ma* X Ma* fm Mc Men Ms delO18 fr Mr Sr 87Sr/86Sr Nd 143Nd/144Nd Pb 206Pb/204Pb

1.00 1184.00 0.50 450.00 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 312.00 0.706451 23.00 0.512385 15.00 17.00 1.00 1183.27 0.50 450.41 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.86 0.706451 23.00 0.512385 15.00 17.00 1.00 1182.54 0.50 450.82 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.72 0.706451 23.00 0.512385 15.00 17.00 1.00 1181.81 0.50 451.24 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.57 0.706451 23.01 0.512385 15.00 17.00 1.00 1181.09 0.50 451.65 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.41 0.706451 23.01 0.512385 15.00 17.00 1.00 1180.36 0.50 452.07 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.24 0.706451 23.01 0.512385 15.01 17.00 1.00 1179.63 0.50 452.49 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 311.06 0.706451 23.01 0.512385 15.01 17.00 1.00 1178.90 0.50 452.92 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 310.85 0.706451 23.02 0.512385 15.01 17.00 1.00 1178.17 0.50 453.36 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 310.63 0.706451 23.02 0.512385 15.01 17.00 1.00 1177.44 0.50 453.81 1.02 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.02 310.38 0.706451 23.02 0.512385 15.01 17.00 1.00 1176.71 0.50 454.27 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.03 310.11 0.706451 23.02 0.512385 15.01 17.00 0.99 1175.99 0.50 454.75 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.04 309.81 0.706451 23.03 0.512385 15.01 17.00 0.99 1175.26 0.50 455.24 1.04 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.05 309.49 0.706451 23.03 0.512385 15.02 17.00 0.99 1174.53 0.50 455.75 1.05 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.06 309.14 0.706451 23.03 0.512385 15.02 17.00 0.99 1173.80 0.50 456.28 1.07 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.07 308.78 0.706451 23.04 0.512385 15.02 17.00 0.99 1173.07 0.50 456.82 1.08 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.08 308.41 0.706451 23.04 0.512385 15.02 17.00 0.99 1172.34 0.50 457.38 1.09 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.09 308.04 0.706451 23.04 0.512385 15.02 17.00 0.99 1171.61 0.50 457.94 1.10 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.11 307.68 0.706451 23.05 0.512385 15.03 17.00 0.99 1170.89 0.50 458.52 1.12 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.12 307.32 0.706451 23.05 0.512385 15.03 17.00 0.99 1170.16 0.50 459.09 1.13 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.13 306.98 0.706451 23.05 0.512385 15.03 17.00 0.99 1169.43 0.50 459.67 1.14 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.14 306.65 0.706451 23.06 0.512385 15.03 17.00 0.99 1168.70 0.50 460.24 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.15 306.34 0.706451 23.06 0.512385 15.03 17.00 0.99 1167.97 0.50 460.81 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.16 306.04 0.706451 23.07 0.512385 15.04 17.00 0.99 1167.24 0.50 461.38 1.16 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 305.76 0.706451 23.07 0.512385 15.04 17.00 0.99 1166.51 0.50 461.94 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 305.48 0.706451 23.07 0.512385 15.04 17.00 0.99 1165.79 0.50 462.50 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 305.22 0.706451 23.08 0.512385 15.04 17.00 0.99 1165.06 0.51 463.05 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 304.96 0.706451 23.08 0.512385 15.04 17.00 0.99 1164.33 0.51 463.60 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 304.71 0.706451 23.08 0.512385 15.04 17.00 0.99 1163.60 0.51 464.14 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.19 304.47 0.706451 23.09 0.512385 15.05 17.00 0.99 1162.87 0.51 464.68 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 304.22 0.706451 23.09 0.512385 15.05 17.00 0.99 1162.14 0.51 465.23 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 303.98 0.706451 23.09 0.512385 15.05 17.00 0.98 1161.41 0.51 465.77 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 303.74 0.706451 23.10 0.512385 15.05 17.00 0.98 1160.69 0.51 466.31 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 303.49 0.706451 23.10 0.512385 15.05 17.00 0.98 1159.96 0.51 466.86 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 303.24 0.706451 23.10 0.512385 15.06 17.00 0.98 1159.23 0.51 467.41 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 302.98 0.706451 23.11 0.512385 15.06 17.00 0.98 1158.50 0.51 467.97 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 302.71 0.706451 23.11 0.512385 15.06 17.00 0.98 1157.77 0.51 468.54 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 302.44 0.706451 23.11 0.512385 15.06 17.00 0.98 1157.04 0.51 469.12 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 302.15 0.706451 23.12 0.512385 15.06 17.00 0.98 1156.31 0.51 469.72 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 301.85 0.706451 23.12 0.512385 15.07 17.00 0.98 1155.59 0.51 470.34 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 301.54 0.706451 23.13 0.512385 15.07 17.00 0.98 1154.86 0.51 470.97 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 301.22 0.706451 23.13 0.512385 15.07 17.00 0.98 1154.13 0.51 471.62 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.23 300.89 0.706451 23.14 0.512385 15.07 17.00 0.98 1153.40 0.51 472.28 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 300.55 0.706451 23.14 0.512385 15.08 17.00 0.98 1152.67 0.51 472.96 1.23 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 300.20 0.706451 23.14 0.512385 15.08 17.00 0.98 1151.94 0.51 473.63 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.25 299.85 0.706451 23.15 0.512385 15.08 17.00 0.98 1151.21 0.51 474.32 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 299.50 0.706451 23.15 0.512385 15.08 17.00 0.98 1150.49 0.51 475.00 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 299.15 0.706451 23.16 0.512385 15.09 17.00 0.98 1149.76 0.51 475.67 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 298.80 0.706451 23.16 0.512385 15.09 17.00 0.98 1149.03 0.51 476.34 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 298.46 0.706451 23.17 0.512385 15.09 17.00 0.98 1148.30 0.51 477.01 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 298.11 0.706451 23.17 0.512385 15.09 17.00 0.98 1147.57 0.52 477.66 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 297.77 0.706451 23.18 0.512385 15.10 17.00 0.97 1146.84 0.52 478.31 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 297.43 0.706451 23.18 0.512385 15.10 17.00 0.97 1146.11 0.52 478.95 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.29 297.08 0.706451 23.19 0.512385 15.10 17.00 0.97 1145.39 0.52 479.59 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.74 0.706451 23.19 0.512385 15.10 17.00 0.97 1144.66 0.52 480.22 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.40 0.706451 23.20 0.512385 15.11 17.00 0.97 1143.93 0.52 480.84 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.05 0.706451 23.20 0.512385 15.11 17.00 0.97 1143.20 0.52 481.46 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 295.70 0.706451 23.21 0.512385 15.11 17.00 0.97 1142.47 0.52 482.08 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 295.35 0.706451 23.21 0.512385 15.12 17.00 0.97 1141.74 0.52 482.69 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 295.00 0.706451 23.22 0.512385 15.12 17.00 0.97 1141.01 0.52 483.31 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 294.64 0.706451 23.23 0.512385 15.12 17.00 0.97 1140.29 0.52 483.92 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 294.27 0.706451 23.23 0.512385 15.13 17.00 0.97 1139.56 0.52 484.53 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.91 0.706451 23.24 0.512385 15.13 17.00 0.97 1138.83 0.52 485.14 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.53 0.706451 23.24 0.512385 15.13 17.00 0.97 1138.10 0.52 485.75 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.15 0.706451 23.25 0.512385 15.13 17.00 0.97 1137.37 0.52 486.36 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 292.77 0.706451 23.25 0.512385 15.14 17.00 0.97 1136.64 0.52 486.97 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 292.38 0.706451 23.26 0.512385 15.14 17.00 0.97 1135.91 0.52 487.58 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 291.98 0.706451 23.27 0.512385 15.14 17.00 0.97 1135.19 0.52 488.20 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 291.58 0.706451 23.27 0.512385 15.15 17.00 0.97 1134.46 0.52 488.81 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 291.17 0.706451 23.28 0.512385 15.15 17.00 0.97 1133.73 0.52 489.43 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 290.75 0.706451 23.29 0.512385 15.16 17.00 0.97 1133.00 0.52 490.04 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 290.33 0.706451 23.29 0.512385 15.16 17.00

131 0.96 1132.27 0.52 490.66 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.90 0.706451 23.30 0.512385 15.16 17.00 0.96 1131.54 0.52 491.29 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.46 0.706451 23.31 0.512385 15.17 17.00 0.96 1130.81 0.53 491.91 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.01 0.706451 23.31 0.512385 15.17 17.00 0.96 1130.09 0.53 492.53 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 288.56 0.706451 23.32 0.512385 15.17 17.00 0.96 1129.36 0.53 493.16 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 288.10 0.706451 23.33 0.512385 15.18 17.00 0.96 1128.63 0.53 493.79 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 287.64 0.706451 23.34 0.512385 15.18 17.00 0.96 1127.90 0.53 494.42 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 287.16 0.706451 23.34 0.512385 15.19 17.00 0.96 1127.17 0.53 495.06 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 286.68 0.706451 23.35 0.512385 15.19 17.00 0.96 1126.44 0.53 495.69 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 286.19 0.706451 23.36 0.512385 15.20 17.00 0.96 1125.71 0.53 496.33 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 285.69 0.706451 23.37 0.512385 15.20 17.00 0.96 1124.99 0.53 496.97 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 285.19 0.706451 23.38 0.512385 15.20 17.00 0.96 1124.26 0.53 497.62 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 284.68 0.706451 23.39 0.512385 15.21 17.00 0.96 1123.53 0.53 498.26 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 284.15 0.706451 23.39 0.512385 15.21 17.00 0.96 1122.80 0.53 498.91 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 283.62 0.706451 23.40 0.512385 15.22 17.00 0.96 1122.07 0.53 499.56 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.05 5.80 0.97 0.30 283.08 0.706451 23.41 0.512385 15.22 17.00 0.96 1121.34 0.53 500.22 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 282.54 0.706451 23.42 0.512385 15.23 17.00 0.96 1120.61 0.53 500.87 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 281.98 0.706451 23.43 0.512385 15.23 17.00 0.96 1119.88 0.53 501.53 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 281.41 0.706451 23.44 0.512385 15.24 17.00 0.96 1119.16 0.53 502.19 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 280.84 0.706451 23.45 0.512385 15.24 17.00 0.96 1118.43 0.53 502.86 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 280.26 0.706451 23.46 0.512385 15.25 17.00 0.95 1117.70 0.53 503.53 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 279.66 0.706451 23.47 0.512385 15.25 17.00 0.95 1116.97 0.53 504.20 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 279.06 0.706451 23.48 0.512385 15.26 17.00 0.95 1116.24 0.53 504.87 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 278.45 0.706451 23.49 0.512385 15.27 17.00 0.95 1115.51 0.53 505.55 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 277.83 0.706451 23.50 0.512385 15.27 17.00 0.95 1114.78 0.53 506.23 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 277.20 0.706451 23.51 0.512385 15.28 17.00 0.95 1114.06 0.54 506.91 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 276.56 0.706451 23.52 0.512385 15.28 17.00 0.95 1113.33 0.54 507.59 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 275.91 0.706451 23.53 0.512385 15.29 17.00 0.95 1112.60 0.54 508.28 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 275.25 0.706451 23.54 0.512385 15.29 17.00 0.95 1111.87 0.54 508.98 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 274.58 0.706451 23.55 0.512385 15.30 17.00 0.95 1111.14 0.54 509.67 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 273.90 0.706451 23.57 0.512385 15.31 17.00 0.95 1110.41 0.54 510.37 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 273.21 0.706451 23.58 0.512385 15.31 17.00 0.95 1109.68 0.54 511.07 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 272.50 0.706451 23.59 0.512385 15.32 17.00 0.95 1108.96 0.54 511.78 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 271.79 0.706451 23.60 0.512385 15.33 17.00 0.95 1108.23 0.54 512.49 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 271.07 0.706451 23.62 0.512385 15.33 17.00 0.95 1107.50 0.54 513.20 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 270.34 0.706451 23.63 0.512385 15.34 17.00 0.95 1106.77 0.54 513.92 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 269.59 0.706451 23.64 0.512385 15.35 17.00 0.95 1106.04 0.54 514.64 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 268.84 0.706451 23.65 0.512385 15.35 17.00 0.95 1105.31 0.54 515.36 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 268.07 0.706451 23.67 0.512385 15.36 17.00 0.95 1104.58 0.54 516.09 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 267.29 0.706451 23.68 0.512385 15.37 17.00 0.95 1103.86 0.54 516.82 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 266.50 0.706451 23.70 0.512385 15.38 17.00 0.94 1103.13 0.54 517.55 1.24 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 265.70 0.706451 23.71 0.512385 15.38 17.00 0.94 1102.40 0.54 518.29 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 264.89 0.706451 23.72 0.512385 15.39 17.00 0.94 1101.67 0.54 519.04 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 264.06 0.706451 23.74 0.512385 15.40 17.00 0.94 1100.94 0.54 519.78 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 263.23 0.706451 23.75 0.512385 15.41 17.00 0.94 1100.21 0.54 520.53 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 262.38 0.706451 23.77 0.512385 15.42 17.00 0.94 1099.48 0.55 521.29 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 261.52 0.706451 23.79 0.512385 15.43 17.00 0.94 1098.76 0.55 522.05 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 260.65 0.706451 23.80 0.512385 15.43 17.00 0.94 1098.03 0.55 522.81 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 259.76 0.706451 23.82 0.512385 15.44 17.00 0.94 1097.30 0.55 523.58 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 258.86 0.706451 23.83 0.512385 15.45 17.00 0.94 1096.57 0.55 524.35 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 257.95 0.706451 23.85 0.512385 15.46 17.00 0.94 1095.84 0.55 525.13 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 257.03 0.706451 23.87 0.512385 15.47 17.00 0.94 1095.11 0.55 525.91 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 256.10 0.706451 23.89 0.512385 15.48 17.00 0.94 1094.38 0.55 526.70 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 255.15 0.706451 23.90 0.512385 15.49 17.00 0.94 1093.66 0.55 527.49 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 254.19 0.706451 23.92 0.512385 15.50 17.00 0.94 1092.93 0.55 528.28 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 253.22 0.706451 23.94 0.512385 15.51 17.00 0.94 1092.20 0.55 529.08 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 252.23 0.706451 23.96 0.512385 15.52 17.00 0.94 1091.47 0.55 529.89 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 251.23 0.706451 23.98 0.512385 15.53 17.00 0.94 1090.74 0.55 530.70 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.10 5.80 0.93 0.30 250.22 0.706451 24.00 0.512385 15.54 17.00 0.94 1090.01 0.55 531.51 1.21 0.00 0.00 0.00 0.92 0.09 0.00 0.10 5.80 0.92 0.30 249.19 0.706451 24.02 0.512385 15.55 17.00 0.94 1089.28 0.55 532.33 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 248.15 0.706451 24.04 0.512385 15.56 17.00 0.93 1088.56 0.55 533.16 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 247.10 0.706451 24.06 0.512385 15.57 17.00 0.93 1087.83 0.55 533.99 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 246.04 0.706451 24.08 0.512385 15.58 17.00 0.93 1087.10 0.55 534.82 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 244.96 0.706451 24.10 0.512385 15.59 17.00 0.93 1086.37 0.56 535.66 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 243.86 0.706451 24.12 0.512385 15.61 17.00 0.93 1085.64 0.56 536.51 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 242.76 0.706451 24.14 0.512385 15.62 17.00 0.93 1084.91 0.56 537.36 1.20 0.00 0.00 0.00 0.92 0.11 0.00 0.11 5.80 0.92 0.30 241.63 0.706451 24.16 0.512385 15.63 17.00 0.93 1084.18 0.56 538.22 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 240.50 0.706451 24.19 0.512385 15.64 17.00 0.93 1083.46 0.56 539.08 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 239.35 0.706451 24.21 0.512385 15.66 17.00 0.93 1082.73 0.56 539.95 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 238.19 0.706451 24.23 0.512385 15.67 17.00 0.93 1082.00 0.56 540.82 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 237.01 0.706451 24.26 0.512385 15.68 17.00 0.93 1081.27 0.56 541.70 1.19 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 235.82 0.706451 24.28 0.512385 15.69 17.00 0.93 1080.54 0.56 542.58 1.18 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 234.62 0.706451 24.31 0.512385 15.71 17.00 0.93 1079.81 0.56 543.48 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.12 5.80 0.90 0.30 233.40 0.706451 24.33 0.512385 15.72 17.00 0.93 1079.08 0.56 544.37 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 232.17 0.706451 24.36 0.512385 15.73 17.00 0.93 1078.36 0.56 545.27 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 230.92 0.706451 24.38 0.512385 15.75 17.00 0.93 1077.63 0.56 546.18 1.18 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 229.66 0.706451 24.41 0.512385 15.76 17.00 0.93 1076.90 0.56 547.10 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 228.39 0.706451 24.44 0.512385 15.78 17.00 0.93 1076.17 0.56 548.02 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 227.10 0.706451 24.47 0.512385 15.79 17.00 0.93 1075.44 0.56 548.95 1.17 0.00 0.00 0.00 0.89 0.13 0.00 0.14 5.80 0.89 0.30 225.80 0.706451 24.49 0.512385 15.81 17.00 0.93 1074.71 0.56 549.88 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 224.48 0.706451 24.52 0.512385 15.82 17.00 0.92 1073.98 0.57 550.82 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 223.15 0.706451 24.55 0.512385 15.84 17.00 0.92 1073.26 0.57 551.77 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 221.81 0.706451 24.58 0.512385 15.85 17.00 0.92 1072.53 0.57 552.72 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.15 5.80 0.89 0.30 220.45 0.706451 24.61 0.512385 15.87 17.00 0.92 1071.80 0.57 553.68 1.16 0.00 0.00 0.00 0.89 0.15 0.00 0.15 5.80 0.89 0.30 219.08 0.706451 24.64 0.512385 15.89 17.00 0.92 1071.07 0.57 554.64 1.16 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 217.69 0.706451 24.67 0.512385 15.90 17.00 0.92 1070.34 0.57 555.62 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 216.29 0.706451 24.71 0.512385 15.92 17.00 0.92 1069.61 0.57 556.60 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.16 5.80 0.88 0.30 214.88 0.706451 24.74 0.512385 15.94 17.00 0.92 1068.88 0.57 557.58 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 213.45 0.706451 24.77 0.512385 15.96 17.00 0.92 1068.16 0.57 558.58 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 212.01 0.706451 24.81 0.512385 15.97 17.00 0.92 1067.43 0.57 559.58 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.16 5.80 0.87 0.30 210.56 0.706451 24.84 0.512385 15.99 17.00 0.92 1066.70 0.57 560.58 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.17 5.80 0.87 0.30 209.09 0.706451 24.87 0.512385 16.01 17.00 0.92 1065.97 0.57 561.60 1.14 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 207.61 0.706451 24.91 0.512385 16.03 17.00 0.92 1065.24 0.57 562.62 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 206.11 0.706451 24.95 0.512385 16.05 17.00

132 0.92 1064.51 0.57 563.65 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.18 5.80 0.87 0.30 204.61 0.706451 24.98 0.512385 16.07 17.00 0.92 1063.78 0.57 564.68 1.13 0.00 0.00 0.00 0.86 0.17 0.00 0.18 5.80 0.86 0.30 203.09 0.706451 25.02 0.512385 16.09 17.00 0.92 1063.06 0.58 565.72 1.13 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 201.55 0.706451 25.06 0.512385 16.11 17.00 0.92 1062.33 0.58 566.77 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 200.01 0.706451 25.10 0.512385 16.13 17.00 0.92 1061.60 0.58 567.83 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.19 5.80 0.86 0.30 198.45 0.706451 25.14 0.512385 16.15 17.00 0.92 1060.87 0.58 568.90 1.12 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 196.88 0.706451 25.18 0.512385 16.17 17.00 0.92 1060.14 0.58 569.97 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 195.30 0.706451 25.22 0.512385 16.19 17.00 0.91 1059.41 0.58 571.05 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 193.70 0.706451 25.26 0.512385 16.22 17.00 0.91 1058.68 0.58 572.13 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 192.09 0.706451 25.30 0.512385 16.24 17.00 0.91 1057.96 0.58 573.23 1.11 0.00 0.00 0.00 0.85 0.20 0.00 0.20 5.80 0.85 0.30 190.48 0.706451 25.34 0.512385 16.26 17.00 0.91 1057.23 0.58 574.33 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.20 5.80 0.84 0.30 188.85 0.706451 25.39 0.512385 16.29 17.00 0.91 1056.50 0.58 575.44 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.21 5.80 0.84 0.30 187.20 0.706451 25.43 0.512385 16.31 17.00 0.91 1055.77 0.58 576.56 1.10 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 185.55 0.706451 25.48 0.512385 16.33 17.00 0.91 1055.04 0.58 577.69 1.09 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 183.89 0.706451 25.52 0.512385 16.36 17.00 0.91 1054.31 0.58 578.82 1.09 0.00 0.00 0.00 0.83 0.21 0.00 0.22 5.80 0.83 0.30 182.22 0.706451 25.57 0.512385 16.38 17.00 0.91 1053.58 0.59 579.96 1.09 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 180.53 0.706451 25.62 0.512385 16.41 17.00 0.91 1052.86 0.59 581.11 1.08 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 178.84 0.706451 25.66 0.512385 16.43 17.00 0.91 1052.13 0.59 582.27 1.08 0.00 0.00 0.00 0.82 0.22 0.00 0.23 5.80 0.82 0.30 177.13 0.706451 25.71 0.512385 16.46 17.00 0.91 1051.40 0.59 583.43 1.08 0.00 0.00 0.00 0.82 0.23 0.00 0.23 5.80 0.82 0.30 175.42 0.706451 25.76 0.512385 16.49 17.00 0.91 1050.67 0.59 584.60 1.07 0.00 0.00 0.00 0.82 0.23 0.00 0.24 5.80 0.82 0.30 173.70 0.706451 25.81 0.512385 16.51 17.00 0.91 1049.94 0.59 585.79 1.07 0.00 0.00 0.00 0.82 0.24 0.00 0.24 5.80 0.82 0.30 171.97 0.706451 25.87 0.512385 16.54 17.00 0.91 1049.21 0.59 586.97 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.24 5.80 0.81 0.30 170.23 0.706451 25.92 0.512385 16.57 17.00 0.91 1048.48 0.59 588.17 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.25 5.80 0.81 0.30 168.48 0.706451 25.97 0.512385 16.60 17.00 0.91 1047.76 0.59 589.38 1.06 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 166.72 0.706451 26.03 0.512385 16.63 17.00 0.91 1047.03 0.59 590.59 1.05 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 164.96 0.706451 26.08 0.512385 16.66 17.00 0.91 1046.30 0.59 591.81 1.05 0.00 0.00 0.00 0.80 0.25 0.00 0.26 5.80 0.80 0.30 163.19 0.706451 26.14 0.512385 16.69 17.00 0.91 1045.57 0.59 593.04 1.05 0.00 0.00 0.00 0.80 0.26 0.00 0.26 5.80 0.80 0.30 161.41 0.706451 26.20 0.512385 16.72 17.00 0.90 1044.84 0.60 594.28 1.04 0.00 0.00 0.00 0.80 0.26 0.00 0.27 5.80 0.80 0.30 159.62 0.706451 26.26 0.512385 16.75 17.00 0.90 1044.11 0.60 595.52 1.04 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 157.83 0.706451 26.31 0.512385 16.78 17.00 0.90 1043.38 0.60 596.78 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 156.04 0.706451 26.38 0.512385 16.81 17.00 0.90 1042.66 0.60 598.04 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.28 5.80 0.79 0.30 154.23 0.706451 26.44 0.512385 16.84 17.00 0.90 1041.93 0.60 599.31 1.03 0.00 0.00 0.00 0.78 0.28 0.00 0.28 5.80 0.78 0.30 152.43 0.706451 26.50 0.512385 16.88 17.00 0.90 1041.20 0.60 600.59 1.02 0.00 0.00 0.00 0.78 0.28 0.00 0.29 5.80 0.78 0.30 150.62 0.706452 26.56 0.512385 16.91 17.00 0.90 1040.47 0.60 601.87 1.02 0.00 0.00 0.00 0.78 0.29 0.00 0.29 5.80 0.78 0.30 148.80 0.706452 26.63 0.512385 16.95 17.00 0.90 1039.74 0.60 603.17 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.29 5.80 0.77 0.30 146.98 0.706452 26.69 0.512385 16.98 17.00 0.90 1039.01 0.60 604.47 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.30 5.80 0.77 0.30 145.16 0.706452 26.76 0.512385 17.02 17.00 0.90 1038.28 0.60 605.78 1.01 0.00 0.00 0.00 0.77 0.30 0.00 0.30 5.80 0.77 0.30 143.33 0.706452 26.83 0.512385 17.05 17.00 0.90 1037.56 0.60 607.10 1.00 0.00 0.00 0.00 0.76 0.30 0.00 0.31 5.80 0.76 0.30 141.50 0.706452 26.90 0.512385 17.09 17.00 0.90 1036.83 0.61 608.43 1.00 0.00 0.00 0.00 0.76 0.31 0.00 0.31 5.80 0.76 0.30 139.67 0.706452 26.97 0.512385 17.13 17.00 0.90 1036.10 0.61 609.76 0.99 0.00 0.00 0.00 0.76 0.31 0.00 0.32 5.80 0.76 0.30 137.84 0.706452 27.04 0.512385 17.16 17.00 0.90 1035.37 0.61 611.10 0.99 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 136.00 0.706452 27.11 0.512385 17.20 17.00 0.90 1034.64 0.61 612.45 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 134.17 0.706452 27.19 0.512385 17.24 17.00 0.90 1033.91 0.61 613.81 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.33 5.80 0.75 0.30 132.33 0.706452 27.26 0.512385 17.28 17.00 0.90 1033.18 0.61 615.18 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.33 5.80 0.74 0.30 130.50 0.706452 27.34 0.512385 17.32 17.00 0.90 1032.46 0.61 616.55 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.34 5.80 0.74 0.30 128.66 0.706452 27.41 0.512385 17.36 17.00 0.90 1031.73 0.61 617.93 0.97 0.00 0.00 0.00 0.74 0.34 0.00 0.34 5.80 0.74 0.30 126.83 0.706452 27.49 0.512385 17.40 17.00 0.90 1031.00 0.61 619.32 0.96 0.00 0.00 0.00 0.73 0.34 0.00 0.35 5.80 0.73 0.30 125.00 0.706452 27.57 0.512385 17.45 17.00 0.89 1030.27 0.61 620.72 0.96 0.00 0.00 0.00 0.73 0.35 0.00 0.35 5.80 0.73 0.30 123.17 0.706452 27.66 0.512385 17.49 17.00 0.89 1029.54 0.61 622.12 0.95 0.00 0.00 0.00 0.73 0.35 0.00 0.36 5.80 0.73 0.30 121.34 0.706452 27.74 0.512385 17.53 17.00 0.89 1028.81 0.62 623.54 0.95 0.00 0.00 0.00 0.72 0.36 0.00 0.36 5.80 0.72 0.30 119.52 0.706452 27.82 0.512385 17.58 17.00 0.89 1028.08 0.62 624.96 0.94 0.00 0.00 0.00 0.72 0.36 0.00 0.37 5.80 0.72 0.30 117.70 0.706452 27.91 0.512384 17.62 17.00 0.89 1027.36 0.62 626.38 0.94 0.00 0.00 0.00 0.72 0.37 0.00 0.37 5.80 0.72 0.30 115.88 0.706452 28.00 0.512384 17.67 17.00 0.89 1026.63 0.62 627.82 0.93 0.00 0.00 0.00 0.71 0.37 0.00 0.38 5.80 0.71 0.30 114.07 0.706453 28.08 0.512384 17.71 17.00 0.89 1025.90 0.62 629.26 0.93 0.00 0.00 0.00 0.71 0.38 0.00 0.38 5.80 0.71 0.30 112.26 0.706453 28.17 0.512384 17.76 17.00 0.89 1025.17 0.62 630.71 0.92 0.00 0.00 0.00 0.70 0.38 0.00 0.39 5.80 0.70 0.30 110.46 0.706453 28.27 0.512384 17.81 17.00 0.89 1024.44 0.62 632.17 0.92 0.00 0.00 0.00 0.70 0.39 0.00 0.39 5.80 0.70 0.30 108.67 0.706453 28.36 0.512384 17.86 17.00 0.89 1023.71 0.62 633.63 0.91 0.00 0.00 0.00 0.70 0.39 0.00 0.40 5.80 0.70 0.30 106.88 0.706453 28.45 0.512384 17.91 17.00 0.89 1022.98 0.62 635.10 0.91 0.00 0.00 0.00 0.69 0.40 0.00 0.40 5.80 0.69 0.30 105.10 0.706453 28.55 0.512384 17.96 17.00 0.89 1022.26 0.62 636.58 0.90 0.00 0.00 0.00 0.69 0.40 0.00 0.41 5.80 0.69 0.30 103.32 0.706453 28.65 0.512384 18.01 17.00 0.89 1021.53 0.63 638.06 0.90 0.00 0.00 0.00 0.68 0.41 0.00 0.41 5.80 0.68 0.30 101.56 0.706453 28.75 0.512384 18.06 17.00 0.89 1020.80 0.63 639.55 0.89 0.00 0.00 0.00 0.68 0.41 0.00 0.42 5.80 0.68 0.30 99.80 0.706454 28.85 0.512384 18.11 17.00 0.89 1020.07 0.63 641.05 0.89 0.00 0.00 0.00 0.68 0.42 0.00 0.42 5.80 0.68 0.30 98.05 0.706454 28.95 0.512384 18.17 17.00 0.89 1019.34 0.63 642.55 0.88 0.00 0.00 0.00 0.67 0.42 0.00 0.43 5.80 0.67 0.30 96.31 0.706454 29.05 0.512384 18.22 17.00 0.89 1018.61 0.63 644.06 0.88 0.00 0.00 0.00 0.67 0.43 0.00 0.43 5.80 0.67 0.30 94.58 0.706454 29.16 0.512384 18.28 17.00 0.89 1017.88 0.63 645.58 0.87 0.00 0.00 0.00 0.66 0.43 0.00 0.44 5.80 0.66 0.30 92.86 0.706454 29.27 0.512384 18.33 17.00 0.89 1017.16 0.63 647.10 0.86 0.00 0.00 0.00 0.66 0.44 0.00 0.44 5.80 0.66 0.30 91.15 0.706455 29.38 0.512384 18.39 17.00 0.89 1016.43 0.63 648.63 0.86 0.00 0.00 0.00 0.66 0.44 0.00 0.45 5.80 0.66 0.30 89.46 0.706455 29.49 0.512384 18.45 17.00 0.88 1015.70 0.63 650.16 0.85 0.00 0.00 0.00 0.65 0.45 0.00 0.45 5.80 0.65 0.30 87.77 0.706455 29.60 0.512384 18.50 17.00 0.88 1014.97 0.63 651.70 0.85 0.00 0.00 0.00 0.65 0.46 0.00 0.46 5.80 0.65 0.30 86.10 0.706455 29.72 0.512384 18.56 17.00 0.88 1014.24 0.64 653.25 0.84 0.00 0.00 0.00 0.64 0.46 0.00 0.46 5.80 0.64 0.30 84.43 0.706456 29.83 0.512384 18.62 17.00 0.88 1013.51 0.64 654.80 0.84 0.00 0.00 0.00 0.64 0.47 0.00 0.47 5.80 0.64 0.30 82.79 0.706456 29.95 0.512384 18.69 17.00

133 0.88 1012.78 0.64 656.36 0.83 0.00 0.00 0.00 0.63 0.47 0.00 0.48 5.80 0.63 0.30 81.15 0.706456 30.07 0.512384 18.75 17.00 0.88 1012.06 0.64 657.93 0.83 0.00 0.00 0.00 0.63 0.48 0.00 0.48 5.80 0.63 0.30 79.53 0.706457 30.19 0.512384 18.81 17.00 0.88 1011.33 0.64 659.50 0.82 0.00 0.00 0.00 0.63 0.48 0.00 0.49 5.80 0.63 0.30 77.92 0.706457 30.32 0.512384 18.88 17.00 0.88 1010.60 0.64 661.09 0.82 0.00 0.00 0.00 0.62 0.49 0.00 0.49 5.80 0.62 0.30 76.33 0.706458 30.44 0.512383 18.94 17.00 0.88 1009.87 0.64 662.69 0.81 0.00 0.00 0.00 0.62 0.49 0.00 0.50 5.80 0.62 0.30 74.75 0.706458 30.57 0.512383 19.01 17.00 0.88 1009.14 0.64 664.31 0.80 0.00 0.00 0.00 0.61 0.50 0.00 0.50 5.80 0.61 0.30 73.19 0.706459 30.70 0.512383 19.07 17.00 0.88 1008.41 0.64 665.96 0.80 0.00 0.00 0.00 0.61 0.51 0.00 0.51 5.80 0.61 0.30 71.64 0.706459 30.83 0.512383 19.14 17.00 0.88 1007.68 0.65 667.64 0.79 0.00 0.00 0.00 0.60 0.51 0.00 0.52 5.80 0.60 0.30 70.11 0.706460 30.97 0.512383 19.21 17.00 0.88 1006.96 0.65 669.37 0.79 0.00 0.00 0.00 0.60 0.52 0.00 0.52 5.80 0.60 0.30 68.59 0.706461 31.11 0.512383 19.28 17.00 0.88 1006.23 0.65 671.16 0.78 0.00 0.00 0.00 0.60 0.52 0.01 0.53 5.80 0.60 0.30 67.09 0.706461 31.24 0.512383 19.35 17.00 0.88 1005.50 0.65 673.04 0.78 0.00 0.00 0.00 0.59 0.53 0.01 0.54 5.80 0.59 0.30 65.60 0.706462 31.39 0.512383 19.43 17.00 0.88 1004.77 0.65 675.03 0.77 0.00 0.00 0.00 0.59 0.54 0.01 0.54 5.80 0.59 0.31 64.13 0.706463 31.53 0.512383 19.50 17.00 0.88 1004.04 0.65 677.18 0.77 0.00 0.00 0.00 0.58 0.54 0.01 0.55 5.80 0.58 0.31 62.68 0.706465 31.67 0.512383 19.57 17.00 0.88 1003.31 0.65 679.52 0.77 0.00 0.00 0.00 0.58 0.55 0.01 0.56 5.80 0.58 0.31 61.24 0.706466 31.82 0.512382 19.65 17.00 0.88 1002.58 0.66 682.08 0.76 0.00 0.00 0.00 0.57 0.55 0.01 0.57 5.80 0.57 0.32 59.82 0.706468 31.98 0.512382 19.73 17.00 0.88 1001.86 0.66 684.89 0.76 0.00 0.00 0.00 0.57 0.56 0.02 0.58 5.79 0.57 0.33 58.41 0.706470 32.13 0.512382 19.80 17.01 0.87 1001.13 0.66 687.99 0.76 0.00 0.00 0.00 0.56 0.56 0.02 0.59 5.79 0.56 0.33 57.02 0.706473 32.29 0.512382 19.88 17.01 0.87 1000.40 0.66 691.36 0.76 0.00 0.00 0.00 0.56 0.57 0.02 0.60 5.79 0.56 0.34 55.64 0.706476 32.45 0.512381 19.96 17.01 0.87 999.67 0.66 695.00 0.76 0.00 0.00 0.00 0.55 0.58 0.03 0.61 5.79 0.55 0.35 54.29 0.706480 32.61 0.512381 20.05 17.01 0.87 998.94 0.67 698.85 0.76 0.00 0.00 0.00 0.55 0.58 0.04 0.62 5.79 0.55 0.37 52.95 0.706484 32.78 0.512380 20.13 17.01 0.87 998.21 0.67 702.86 0.76 0.00 0.00 0.00 0.55 0.59 0.04 0.63 5.79 0.55 0.38 51.63 0.706490 32.95 0.512380 20.21 17.01 0.87 997.48 0.67 706.95 0.76 0.00 0.00 0.00 0.54 0.60 0.05 0.64 5.79 0.54 0.39 50.33 0.706497 33.12 0.512379 20.30 17.01 0.87 996.75 0.68 711.05 0.76 0.00 0.00 0.00 0.54 0.60 0.05 0.66 5.79 0.54 0.40 49.06 0.706504 33.30 0.512379 20.39 17.01 0.87 996.03 0.68 715.09 0.76 0.00 0.00 0.00 0.53 0.61 0.06 0.67 5.79 0.53 0.42 47.80 0.706513 33.48 0.512378 20.47 17.01 0.87 995.30 0.68 719.01 0.76 0.00 0.00 0.00 0.53 0.62 0.06 0.68 5.79 0.53 0.43 46.57 0.706523 33.66 0.512377 20.56 17.01 0.87 994.57 0.68 722.76 0.76 0.00 0.00 0.00 0.52 0.62 0.07 0.69 5.78 0.52 0.44 45.37 0.706533 33.84 0.512376 20.65 17.02 0.87 993.84 0.69 726.33 0.76 0.00 0.00 0.00 0.52 0.63 0.07 0.70 5.78 0.52 0.45 44.19 0.706545 34.03 0.512375 20.74 17.02 0.87 993.11 0.69 729.70 0.76 0.00 0.00 0.00 0.51 0.64 0.08 0.71 5.78 0.51 0.46 43.03 0.706558 34.23 0.512374 20.84 17.02 0.87 992.38 0.69 732.87 0.76 0.00 0.00 0.00 0.51 0.64 0.08 0.72 5.78 0.51 0.46 41.89 0.706571 34.42 0.512373 20.93 17.02 0.87 991.65 0.69 735.85 0.75 0.00 0.00 0.00 0.50 0.65 0.08 0.73 5.78 0.50 0.47 40.78 0.706585 34.62 0.512372 21.03 17.02 0.87 990.93 0.69 738.65 0.75 0.00 0.00 0.00 0.50 0.66 0.09 0.74 5.77 0.50 0.48 39.69 0.706600 34.82 0.512371 21.12 17.02 0.87 990.20 0.70 741.31 0.74 0.00 0.00 0.00 0.49 0.66 0.09 0.75 5.77 0.49 0.48 38.62 0.706616 35.02 0.512370 21.22 17.03 0.87 989.47 0.70 743.82 0.74 0.00 0.00 0.00 0.49 0.67 0.09 0.76 5.77 0.49 0.48 37.58 0.706633 35.23 0.512369 21.32 17.03 0.87 988.74 0.70 746.21 0.73 0.00 0.00 0.00 0.49 0.68 0.09 0.77 5.77 0.49 0.49 36.55 0.706652 35.44 0.512368 21.42 17.03 0.87 988.01 0.70 748.51 0.73 0.00 0.00 0.00 0.48 0.68 0.09 0.77 5.76 0.48 0.49 35.55 0.706671 35.65 0.512367 21.52 17.03 0.87 987.28 0.70 750.71 0.72 0.00 0.01 0.01 0.48 0.69 0.09 0.78 5.76 0.48 0.49 34.57 0.706691 35.86 0.512365 21.62 17.03 0.86 986.55 0.70 752.84 0.72 0.00 0.01 0.01 0.47 0.70 0.09 0.79 5.76 0.47 0.49 33.61 0.706713 36.08 0.512364 21.72 17.04 0.86 985.83 0.71 754.91 0.71 0.00 0.01 0.01 0.47 0.70 0.09 0.80 5.76 0.47 0.49 32.67 0.706736 36.30 0.512363 21.83 17.04 0.86 985.10 0.71 756.93 0.71 0.00 0.01 0.01 0.46 0.71 0.09 0.81 5.75 0.46 0.49 31.76 0.706761 36.53 0.512361 21.93 17.04 0.86 984.37 0.71 758.90 0.70 0.00 0.01 0.01 0.46 0.72 0.09 0.81 5.75 0.46 0.50 30.86 0.706788 36.76 0.512360 22.04 17.04 0.86 983.64 0.71 760.83 0.69 0.00 0.01 0.01 0.45 0.72 0.10 0.82 5.75 0.45 0.50 29.98 0.706817 36.99 0.512358 22.15 17.05 0.86 982.91 0.71 762.73 0.69 0.00 0.01 0.01 0.45 0.73 0.10 0.83 5.75 0.45 0.50 29.13 0.706849 37.23 0.512357 22.26 17.05 0.86 982.18 0.71 764.61 0.68 0.00 0.01 0.01 0.44 0.74 0.10 0.83 5.74 0.44 0.50 28.29 0.706883 37.47 0.512355 22.37 17.05 0.86 981.45 0.71 766.46 0.67 0.00 0.01 0.01 0.44 0.75 0.10 0.84 5.74 0.44 0.50 27.48 0.706919 37.71 0.512354 22.48 17.05 0.86 980.73 0.71 768.29 0.67 0.00 0.01 0.01 0.44 0.75 0.10 0.85 5.73 0.44 0.50 26.69 0.706959 37.96 0.512352 22.60 17.06 0.86 980.00 0.72 770.09 0.66 0.00 0.01 0.01 0.43 0.76 0.10 0.85 5.73 0.43 0.50 25.91 0.707002 38.21 0.512350 22.71 17.06 0.86 979.27 0.72 771.89 0.66 0.00 0.01 0.01 0.43 0.77 0.10 0.86 5.73 0.43 0.50 25.16 0.707048 38.46 0.512348 22.83 17.06 0.86 978.54 0.72 773.66 0.65 0.00 0.01 0.01 0.42 0.77 0.10 0.87 5.72 0.42 0.50 24.43 0.707098 38.72 0.512346 22.94 17.07 0.86 977.81 0.72 775.42 0.64 0.01 0.01 0.01 0.42 0.78 0.10 0.88 5.72 0.42 0.50 23.72 0.707153 38.99 0.512344 23.06 17.07 0.86 977.08 0.72 777.17 0.64 0.01 0.01 0.01 0.41 0.79 0.10 0.88 5.71 0.41 0.50 23.03 0.707212 39.25 0.512342 23.18 17.08 0.86 976.35 0.72 778.90 0.63 0.01 0.01 0.01 0.41 0.79 0.10 0.89 5.71 0.41 0.50 22.35 0.707276 39.53 0.512340 23.30 17.08 0.86 975.63 0.72 780.62 0.63 0.01 0.01 0.01 0.40 0.80 0.10 0.90 5.70 0.40 0.50 21.70 0.707345 39.80 0.512337 23.43 17.08 0.86 974.90 0.72 782.33 0.62 0.01 0.01 0.01 0.40 0.81 0.10 0.90 5.70 0.40 0.50 21.07 0.707419 40.08 0.512335 23.55 17.09 0.86 974.17 0.73 784.02 0.61 0.01 0.01 0.01 0.39 0.81 0.10 0.91 5.69 0.39 0.50 20.46 0.707500 40.37 0.512332 23.67 17.09 0.86 973.44 0.73 785.71 0.61 0.01 0.01 0.01 0.39 0.82 0.10 0.92 5.68 0.39 0.50 19.86 0.707587 40.65 0.512329 23.80 17.10 0.86 972.71 0.73 787.38 0.60 0.01 0.02 0.02 0.39 0.83 0.10 0.92 5.68 0.39 0.50 19.29 0.707680 40.95 0.512327 23.93 17.10 0.85 971.98 0.73 789.04 0.60 0.01 0.02 0.02 0.38 0.83 0.10 0.93 5.67 0.38 0.50 18.73 0.707781 41.24 0.512324 24.05 17.11 0.85 971.25 0.73 790.68 0.59 0.01 0.02 0.02 0.38 0.84 0.10 0.94 5.66 0.38 0.50 18.19 0.707890 41.55 0.512321 24.18 17.11 0.85 970.53 0.73 792.31 0.58 0.01 0.02 0.02 0.37 0.85 0.10 0.94 5.66 0.37 0.50 17.68 0.708007 41.85 0.512317 24.31 17.12 0.85 969.80 0.73 793.93 0.58 0.01 0.02 0.02 0.37 0.85 0.10 0.95 5.65 0.37 0.50 17.18 0.708133 42.16 0.512314 24.44 17.13 0.85 969.07 0.73 795.54 0.57 0.01 0.02 0.02 0.36 0.86 0.10 0.95 5.64 0.36 0.50 16.69 0.708268 42.48 0.512311 24.58 17.13 0.85 968.34 0.73 797.14 0.57 0.01 0.02 0.02 0.36 0.86 0.10 0.96 5.63 0.36 0.50 16.23 0.708412 42.80 0.512307 24.71 17.14 0.85 967.61 0.74 798.72 0.56 0.01 0.02 0.02 0.36 0.87 0.10 0.97 5.62 0.36 0.50 15.79 0.708567 43.12 0.512304 24.84 17.15 0.85 966.88 0.74 800.28 0.56 0.01 0.02 0.02 0.35 0.88 0.10 0.97 5.61 0.35 0.50 15.36 0.708732 43.45 0.512300 24.98 17.15 0.85 966.15 0.74 801.84 0.55 0.01 0.02 0.02 0.35 0.88 0.10 0.98 5.60 0.35 0.50 14.95 0.708908 43.78 0.512296 25.11 17.16 0.85 965.43 0.74 803.38 0.55 0.01 0.02 0.02 0.34 0.89 0.10 0.99 5.59 0.34 0.50 14.56 0.709095 44.12 0.512292 25.25 17.17 0.85 964.70 0.74 804.90 0.54 0.01 0.03 0.03 0.34 0.90 0.10 0.99 5.58 0.34 0.50 14.18 0.709294 44.46 0.512287 25.39 17.18 0.85 963.97 0.74 806.42 0.54 0.01 0.03 0.03 0.33 0.90 0.10 1.00 5.57 0.33 0.50 13.82 0.709505 44.80 0.512283 25.52 17.18 0.85 963.24 0.74 807.92 0.53 0.01 0.03 0.03 0.33 0.91 0.10 1.00 5.56 0.33 0.50 13.48 0.709729 45.15 0.512279 25.66 17.19 0.85 962.51 0.74 809.40 0.53 0.01 0.03 0.03 0.33 0.91 0.10 1.01 5.55 0.33 0.50 13.16 0.709965 45.51 0.512274 25.80 17.20 0.85 961.78 0.74 810.87 0.52 0.01 0.03 0.03 0.32 0.92 0.10 1.02 5.53 0.32 0.50 12.85 0.710214 45.87 0.512269 25.94 17.21 0.85 961.05 0.74 812.32 0.52 0.02 0.03 0.03 0.32 0.93 0.10 1.02 5.52 0.32 0.50 12.56 0.710476 46.23 0.512264 26.08 17.22 0.85 960.33 0.75 813.76 0.51 0.02 0.03 0.03 0.31 0.93 0.10 1.03 5.51 0.31 0.50 12.28 0.710751 46.59 0.512259 26.22 17.23 0.85 959.60 0.75 815.19 0.51 0.02 0.03 0.03 0.31 0.94 0.10 1.03 5.49 0.31 0.50 12.02 0.711038 46.96 0.512254 26.36 17.24 0.85 958.87 0.75 816.60 0.50 0.02 0.04 0.04 0.31 0.94 0.10 1.04 5.48 0.31 0.50 11.77 0.711338 47.34 0.512249 26.50 17.25 0.85 958.14 0.75 817.99 0.50 0.02 0.04 0.04 0.30 0.95 0.10 1.05 5.46 0.30 0.50 11.54 0.711651 47.71 0.512243 26.64 17.26 0.84 957.41 0.75 819.37 0.49 0.02 0.04 0.04 0.30 0.96 0.10 1.05 5.45 0.30 0.50 11.33 0.711976 48.10 0.512238 26.78 17.27 0.84 956.68 0.75 820.74 0.49 0.02 0.04 0.04 0.30 0.96 0.10 1.06 5.43 0.30 0.50 11.12 0.712312 48.48 0.512232 26.92 17.28 0.84 955.95 0.75 822.09 0.49 0.02 0.04 0.04 0.29 0.97 0.10 1.06 5.41 0.29 0.50 10.94 0.712660 48.87 0.512226 27.06 17.30 0.84 955.23 0.75 823.42 0.48 0.02 0.04 0.04 0.29 0.97 0.10 1.07 5.40 0.29 0.50 10.76 0.713018 49.26 0.512220 27.20 17.31 0.84 954.50 0.75 824.74 0.48 0.02 0.04 0.04 0.28 0.98 0.10 1.08 5.38 0.28 0.50 10.60 0.713386 49.65 0.512214 27.34 17.32 0.84 953.77 0.75 826.05 0.47 0.02 0.05 0.05 0.28 0.98 0.10 1.08 5.36 0.28 0.50 10.46 0.713762 50.05 0.512208 27.48 17.33 0.84 953.04 0.76 827.33 0.47 0.02 0.05 0.05 0.28 0.99 0.10 1.09 5.34 0.28 0.50 10.32 0.714147 50.45 0.512201 27.62 17.34 0.84 952.31 0.76 828.61 0.47 0.02 0.05 0.05 0.27 1.00 0.10 1.09 5.32 0.27 0.50 10.20 0.714539 50.85 0.512195 27.76 17.36 0.84 951.58 0.76 829.87 0.46 0.02 0.05 0.05 0.27 1.00 0.10 1.10 5.30 0.27 0.50 10.09 0.714936 51.26 0.512188 27.89 17.37 0.84 950.85 0.76 831.11 0.46 0.03 0.05 0.05 0.27 1.01 0.10 1.10 5.28 0.27 0.50 10.00 0.715339 51.66 0.512181 28.03 17.39 0.84 950.13 0.76 832.34 0.46 0.03 0.06 0.06 0.26 1.01 0.10 1.11 5.26 0.26 0.50 9.91 0.715744 52.07 0.512175 28.17 17.40 0.84 949.40 0.76 833.55 0.45 0.03 0.06 0.06 0.26 1.02 0.10 1.11 5.24 0.26 0.50 9.84 0.716153 52.48 0.512168 28.30 17.41 0.84 948.67 0.76 834.75 0.45 0.03 0.06 0.06 0.25 1.02 0.10 1.12 5.22 0.25 0.50 9.78 0.716563 52.89 0.512161 28.44 17.43 0.84 947.94 0.76 835.94 0.45 0.03 0.06 0.06 0.25 1.03 0.10 1.12 5.19 0.25 0.50 9.73 0.716972 53.31 0.512153 28.57 17.44 0.84 947.21 0.76 837.11 0.44 0.03 0.06 0.06 0.25 1.03 0.10 1.13 5.17 0.25 0.50 9.69 0.717381 53.72 0.512146 28.70 17.46 0.84 946.48 0.76 838.26 0.44 0.03 0.07 0.07 0.24 1.04 0.10 1.13 5.15 0.24 0.50 9.66 0.717787 54.14 0.512139 28.84 17.47 0.84 945.75 0.76 839.40 0.44 0.03 0.07 0.07 0.24 1.04 0.10 1.14 5.12 0.24 0.50 9.64 0.718190 54.55 0.512131 28.97 17.49 0.84 945.03 0.76 840.53 0.43 0.03 0.07 0.07 0.24 1.05 0.10 1.14 5.10 0.24 0.50 9.63 0.718589 54.97 0.512124 29.09 17.51 0.84 944.30 0.77 841.64 0.43 0.03 0.07 0.07 0.23 1.05 0.10 1.15 5.07 0.23 0.50 9.63 0.718981 55.39 0.512116 29.22 17.52 0.84 943.57 0.77 842.74 0.43 0.04 0.07 0.07 0.23 1.06 0.10 1.15 5.05 0.23 0.50 9.64 0.719368 55.80 0.512109 29.35 17.54 0.83 942.84 0.77 843.82 0.43 0.04 0.08 0.08 0.23 1.06 0.10 1.16 5.02 0.23 0.50 9.66 0.719747 56.22 0.512101 29.47 17.56 0.83 942.11 0.77 844.89 0.42 0.04 0.08 0.08 0.22 1.07 0.10 1.16 5.00 0.22 0.50 9.69 0.720118 56.63 0.512093 29.59 17.57 0.83 941.38 0.77 845.94 0.42 0.04 0.08 0.08 0.22 1.07 0.10 1.17 4.97 0.22 0.50 9.72 0.720481 57.05 0.512085 29.71 17.59 0.83 940.65 0.77 846.99 0.42 0.04 0.08 0.08 0.22 1.08 0.10 1.17 4.94 0.22 0.50 9.76 0.720834 57.46 0.512078 29.83 17.61 0.83 939.93 0.77 848.02 0.42 0.04 0.09 0.09 0.21 1.08 0.10 1.18 4.91 0.21 0.50 9.82 0.721178 57.88 0.512070 29.95 17.62 0.83 939.20 0.77 849.03 0.41 0.04 0.09 0.09 0.21 1.09 0.10 1.18 4.89 0.21 0.50 9.87 0.721511 58.29 0.512062 30.06 17.64

134 0.83 938.47 0.77 850.03 0.41 0.04 0.09 0.09 0.21 1.09 0.10 1.19 4.86 0.21 0.50 9.94 0.721834 58.70 0.512054 30.18 17.66 0.83 937.74 0.77 851.02 0.41 0.04 0.09 0.09 0.21 1.10 0.10 1.19 4.83 0.21 0.50 10.01 0.722146 59.10 0.512046 30.29 17.68 0.83 937.01 0.77 852.00 0.41 0.05 0.10 0.10 0.20 1.10 0.10 1.20 4.80 0.20 0.50 10.09 0.722447 59.51 0.512038 30.40 17.70 0.83 936.28 0.77 852.96 0.41 0.05 0.10 0.10 0.20 1.10 0.10 1.20 4.77 0.20 0.50 10.18 0.722737 59.91 0.512030 30.50 17.72 0.83 935.55 0.77 853.92 0.40 0.05 0.10 0.10 0.20 1.11 0.10 1.21 4.74 0.20 0.50 10.27 0.723015 60.31 0.512021 30.61 17.73 0.83 934.83 0.77 854.86 0.40 0.05 0.10 0.10 0.19 1.11 0.10 1.21 4.71 0.19 0.50 10.37 0.723283 60.71 0.512013 30.71 17.75 0.83 934.10 0.77 855.78 0.40 0.05 0.11 0.11 0.19 1.12 0.10 1.21 4.68 0.19 0.50 10.48 0.723540 61.10 0.512005 30.81 17.77 0.83 933.37 0.78 856.70 0.40 0.05 0.11 0.11 0.19 1.12 0.10 1.22 4.65 0.19 0.50 10.59 0.723786 61.49 0.511997 30.90 17.79 0.83 932.64 0.78 857.60 0.40 0.05 0.11 0.11 0.19 1.13 0.10 1.22 4.62 0.19 0.50 10.70 0.724021 61.88 0.511989 31.00 17.81 0.83 931.91 0.78 858.50 0.40 0.06 0.12 0.12 0.18 1.13 0.10 1.23 4.59 0.18 0.50 10.82 0.724246 62.26 0.511981 31.09 17.83 0.83 931.18 0.78 859.38 0.40 0.06 0.12 0.12 0.18 1.13 0.10 1.23 4.56 0.18 0.50 10.95 0.724461 62.64 0.511973 31.18 17.85 0.83 930.45 0.78 860.25 0.39 0.06 0.12 0.12 0.18 1.14 0.10 1.23 4.53 0.18 0.50 11.08 0.724666 63.01 0.511964 31.26 17.87 0.83 929.73 0.78 861.11 0.39 0.06 0.12 0.12 0.17 1.14 0.10 1.24 4.50 0.17 0.50 11.21 0.724861 63.38 0.511956 31.35 17.89 0.83 929.00 0.78 861.96 0.39 0.06 0.13 0.13 0.17 1.15 0.10 1.24 4.47 0.17 0.50 11.35 0.725047 63.75 0.511948 31.43 17.91 0.82 928.27 0.78 862.79 0.39 0.06 0.13 0.13 0.17 1.15 0.10 1.25 4.44 0.17 0.50 11.50 0.725224 64.11 0.511940 31.50 17.93 0.82 927.54 0.78 863.62 0.39 0.06 0.13 0.13 0.17 1.15 0.10 1.25 4.40 0.17 0.50 11.65 0.725392 64.46 0.511932 31.58 17.95 0.82 926.81 0.78 864.44 0.39 0.06 0.14 0.14 0.16 1.16 0.10 1.25 4.37 0.16 0.50 11.80 0.725551 64.81 0.511924 31.65 17.97 0.82 926.08 0.78 865.25 0.39 0.07 0.14 0.14 0.16 1.16 0.10 1.26 4.34 0.16 0.50 11.95 0.725703 65.15 0.511916 31.72 17.99 0.82 925.35 0.78 866.04 0.39 0.07 0.14 0.14 0.16 1.17 0.10 1.26 4.31 0.16 0.50 12.11 0.725847 65.49 0.511908 31.79 18.01 0.82 924.63 0.78 866.83 0.39 0.07 0.14 0.14 0.16 1.17 0.10 1.27 4.28 0.16 0.50 12.27 0.725984 65.83 0.511900 31.86 18.03 0.82 923.90 0.78 867.61 0.39 0.07 0.15 0.15 0.15 1.17 0.10 1.27 4.25 0.15 0.50 12.44 0.726113 66.15 0.511892 31.92 18.05 0.82 923.17 0.78 868.38 0.39 0.07 0.15 0.15 0.15 1.18 0.10 1.27 4.21 0.15 0.50 12.61 0.726236 66.48 0.511884 31.98 18.07 0.82 922.44 0.78 869.14 0.39 0.07 0.15 0.15 0.15 1.18 0.10 1.28 4.18 0.15 0.50 12.78 0.726353 66.79 0.511876 32.03 18.09 0.82 921.71 0.78 869.89 0.39 0.08 0.16 0.16 0.15 1.18 0.10 1.28 4.15 0.15 0.50 12.96 0.726464 67.10 0.511868 32.09 18.11 0.82 920.98 0.78 870.63 0.38 0.08 0.16 0.16 0.14 1.19 0.10 1.28 4.12 0.14 0.50 13.13 0.726568 67.40 0.511861 32.14 18.13 0.82 920.25 0.79 871.36 0.38 0.08 0.16 0.16 0.14 1.19 0.10 1.29 4.09 0.14 0.50 13.31 0.726668 67.70 0.511853 32.18 18.15 0.82 919.53 0.79 872.09 0.38 0.08 0.17 0.17 0.14 1.19 0.10 1.29 4.06 0.14 0.50 13.50 0.726762 67.99 0.511845 32.23 18.17 0.82 918.80 0.79 872.80 0.38 0.08 0.17 0.17 0.14 1.20 0.10 1.29 4.02 0.14 0.50 13.68 0.726851 68.27 0.511838 32.27 18.19 0.82 918.07 0.79 873.51 0.38 0.08 0.17 0.17 0.14 1.20 0.10 1.30 3.99 0.14 0.50 13.87 0.726935 68.55 0.511830 32.31 18.21 0.82 917.34 0.79 874.21 0.38 0.08 0.18 0.18 0.13 1.20 0.10 1.30 3.96 0.13 0.50 14.06 0.727015 68.82 0.511823 32.35 18.23 0.82 916.61 0.79 874.90 0.38 0.09 0.18 0.18 0.13 1.21 0.10 1.30 3.93 0.13 0.50 14.25 0.727091 69.09 0.511815 32.38 18.25 0.82 915.88 0.79 875.59 0.38 0.09 0.18 0.18 0.13 1.21 0.10 1.31 3.90 0.13 0.50 14.45 0.727163 69.35 0.511808 32.41 18.27 0.82 915.15 0.79 876.26 0.38 0.09 0.19 0.19 0.13 1.21 0.10 1.31 3.87 0.13 0.50 14.64 0.727231 69.60 0.511800 32.44 18.29 0.82 914.43 0.79 876.93 0.38 0.09 0.19 0.19 0.13 1.22 0.10 1.31 3.84 0.13 0.50 14.84 0.727295 69.84 0.511793 32.47 18.31 0.81 913.70 0.79 877.59 0.39 0.09 0.19 0.19 0.12 1.22 0.10 1.32 3.81 0.12 0.50 15.04 0.727356 70.08 0.511786 32.49 18.32 0.81 912.97 0.79 878.25 0.39 0.09 0.20 0.20 0.12 1.22 0.10 1.32 3.78 0.12 0.50 15.25 0.727414 70.31 0.511779 32.52 18.34 0.81 912.24 0.79 878.90 0.39 0.10 0.20 0.20 0.12 1.22 0.10 1.32 3.75 0.12 0.50 15.45 0.727469 70.53 0.511771 32.54 18.36 0.81 911.51 0.79 879.54 0.39 0.10 0.20 0.20 0.12 1.23 0.10 1.32 3.72 0.12 0.50 15.66 0.727521 70.75 0.511764 32.55 18.38 0.81 910.78 0.79 880.17 0.39 0.10 0.21 0.21 0.12 1.23 0.10 1.33 3.69 0.12 0.50 15.87 0.727570 70.96 0.511757 32.57 18.40 0.81 910.05 0.79 880.80 0.39 0.10 0.21 0.21 0.11 1.23 0.10 1.33 3.66 0.11 0.50 16.08 0.727617 71.17 0.511750 32.58 18.42 0.81 909.33 0.79 881.42 0.39 0.10 0.21 0.21 0.11 1.24 0.10 1.33 3.63 0.11 0.50 16.29 0.727662 71.36 0.511743 32.59 18.44 0.81 908.60 0.79 882.04 0.39 0.10 0.22 0.22 0.11 1.24 0.10 1.34 3.60 0.11 0.50 16.50 0.727704 71.55 0.511737 32.59 18.46 0.81 907.87 0.79 882.65 0.39 0.11 0.22 0.22 0.11 1.24 0.10 1.34 3.57 0.11 0.50 16.71 0.727744 71.74 0.511730 32.60 18.48 0.81 907.14 0.79 883.25 0.39 0.11 0.22 0.22 0.11 1.24 0.10 1.34 3.54 0.11 0.50 16.93 0.727782 71.91 0.511723 32.60 18.50 0.81 906.41 0.79 883.85 0.39 0.11 0.23 0.23 0.10 1.25 0.10 1.34 3.51 0.10 0.50 17.15 0.727818 72.08 0.511717 32.60 18.52 0.81 905.68 0.79 884.44 0.39 0.11 0.23 0.23 0.10 1.25 0.10 1.35 3.48 0.10 0.50 17.37 0.727852 72.25 0.511710 32.60 18.54 0.81 904.95 0.79 885.02 0.39 0.11 0.23 0.23 0.10 1.25 0.10 1.35 3.45 0.10 0.50 17.59 0.727885 72.41 0.511703 32.60 18.55 0.81 904.23 0.80 885.60 0.39 0.11 0.24 0.24 0.10 1.25 0.10 1.35 3.43 0.10 0.50 17.81 0.727916 72.56 0.511697 32.59 18.57 0.81 903.50 0.80 886.18 0.40 0.12 0.24 0.24 0.10 1.26 0.10 1.35 3.40 0.10 0.50 18.03 0.727946 72.70 0.511691 32.58 18.59 0.81 902.77 0.80 886.74 0.40 0.12 0.24 0.24 0.10 1.26 0.10 1.36 3.37 0.10 0.50 18.25 0.727974 72.84 0.511684 32.57 18.61 0.81 902.04 0.80 887.31 0.40 0.12 0.25 0.25 0.09 1.26 0.10 1.36 3.34 0.09 0.50 18.48 0.728000 72.98 0.511678 32.56 18.63 0.81 901.31 0.80 887.87 0.40 0.12 0.25 0.25 0.09 1.26 0.10 1.36 3.32 0.09 0.50 18.70 0.728026 73.10 0.511672 32.55 18.65 0.81 900.58 0.80 888.42 0.40 0.12 0.26 0.26 0.09 1.27 0.10 1.36 3.29 0.09 0.50 18.93 0.728050 73.22 0.511666 32.53 18.67 0.81 899.85 0.80 888.97 0.40 0.12 0.26 0.26 0.09 1.27 0.10 1.37 3.26 0.09 0.50 19.16 0.728073 73.34 0.511659 32.52 18.68 0.80 899.13 0.80 889.51 0.40 0.13 0.26 0.26 0.09 1.27 0.10 1.37 3.24 0.09 0.50 19.39 0.728095 73.45 0.511653 32.50 18.70 0.80 898.40 0.80 890.05 0.40 0.13 0.27 0.27 0.09 1.27 0.10 1.37 3.21 0.09 0.50 19.62 0.728116 73.55 0.511647 32.48 18.72 0.80 897.67 0.80 890.59 0.41 0.13 0.27 0.27 0.09 1.28 0.10 1.37 3.19 0.09 0.50 19.85 0.728136 73.65 0.511642 32.46 18.74 0.80 896.94 0.80 891.12 0.41 0.13 0.27 0.27 0.08 1.28 0.10 1.37 3.16 0.08 0.50 20.09 0.728155 73.74 0.511636 32.43 18.75 0.80 896.21 0.80 891.65 0.41 0.13 0.28 0.28 0.08 1.28 0.10 1.38 3.14 0.08 0.50 20.32 0.728173 73.82 0.511630 32.41 18.77 0.80 895.48 0.80 892.17 0.41 0.13 0.28 0.28 0.08 1.28 0.10 1.38 3.11 0.08 0.50 20.56 0.728190 73.90 0.511624 32.38 18.79 0.80 894.75 0.80 892.68 0.41 0.14 0.28 0.28 0.08 1.28 0.10 1.38 3.09 0.08 0.50 20.80 0.728207 73.98 0.511618 32.35 18.81 0.80 894.03 0.80 893.20 0.41 0.14 0.29 0.29 0.08 1.29 0.10 1.38 3.06 0.08 0.50 21.03 0.728223 74.05 0.511613 32.32 18.82

135 EC-RAXFC Results - Melts Page MODEL B

Equilibration Parameters tlm 1184 degC 18O/16O in magma 5.8 Magma a 450 Mro 0.5 Element Name Sr Nd Pb Teq Norm 0.812 tmo 1184 degC 18O/16O in assimilant 0.5 Magma b -11 Episodic Recharge Magma: conc. 312 23 15 Teq deg C 910.05392 tla 1129 degC 18O/16O in recharge 5.8 Assimilant a 400 Episode deltaMri Tm,i mr,i d,i bulk Dmo 4 0.4 0.5 Mm 0.552310517 tao 450 degC Oxygen conc magma 0.47 Assimilant b -11 1 0.2 1000 0.3 2 enthalpy 0 0 0 Mao 1.847974615 tlr 1184 degC Oxygen conc assimilant 0.5 Recharge Magma a 450 2 0.2 1175 0.3 2 Assimilant: conc. 436 38 15 Ma* 0.381622811 tro 1184 degC Oxygen conc recharge 0.47 Recharge Magma b -11 3 0.1 1155 0.3 2 bulk Dao 6 0.6 0.7 Mc 1.232676143 ts 750 degC enthalpy 0 0 0 Men 0.096636151 cpm 1100 J/kg K Recharge: conc. 300 23 15 Ms 1.329312294 cpa 1000 J/kg K bulk Dro 4 0.4 0.5 fa 0.206508687 cpr 1100 J/kg K enthalpy 0 0 0 fm 0.113791804 hm 400000 J/kg Isotope Name 87Sr/86Sr 143Nd/144Nd 206Pb/204Pb fr 0.113791804 ha 350000 J/kg ratio in magma 0.706451 0.512385 17 hr 400000 J/kg ratio in assimilant 0.728666 0.510803 21.9 X 1 Normalized fraction of Wallrock melt ratio in recharge 0.706451 0.512385 17 mixed into Magma body

Norm T T magma Norm T T assim magma (deg C) assim (deg C) Mm fa Ma* X Ma* fm Mc Men Ms delO18 fr Mr Sr 87Sr/86Sr Nd 143Nd/144Nd Pb 206Pb/204Pb

1.00 1184.00 0.50 450.00 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 312.00 0.706451 23.00 0.5123850 15.00 17.00 1.00 1183.27 0.50 450.46 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.86 0.706451 23.00 0.5123850 15.00 17.00 1.00 1182.54 0.50 450.93 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.72 0.706451 23.00 0.5123850 15.00 17.00 1.00 1181.81 0.50 451.40 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.57 0.706451 23.01 0.5123850 15.00 17.00 1.00 1181.09 0.50 451.87 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.41 0.706451 23.01 0.5123850 15.00 17.00 1.00 1180.36 0.50 452.34 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.24 0.706451 23.01 0.5123850 15.01 17.00 1.00 1179.63 0.50 452.82 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 311.06 0.706451 23.01 0.5123850 15.01 17.00 1.00 1178.90 0.50 453.31 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 310.85 0.706451 23.02 0.5123850 15.01 17.00 1.00 1178.17 0.50 453.80 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 310.63 0.706451 23.02 0.5123850 15.01 17.00 1.00 1177.44 0.50 454.31 1.02 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.02 310.38 0.706451 23.02 0.5123850 15.01 17.00 1.00 1176.71 0.50 454.83 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.03 310.11 0.706451 23.02 0.5123850 15.01 17.00 0.99 1175.99 0.50 455.37 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.04 309.81 0.706451 23.03 0.5123850 15.01 17.00 0.99 1175.26 0.50 455.93 1.04 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.05 309.49 0.706451 23.03 0.5123850 15.02 17.00 0.99 1174.53 0.50 456.51 1.05 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.06 309.14 0.706451 23.03 0.5123850 15.02 17.00 0.99 1173.80 0.50 457.10 1.07 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.07 308.78 0.706451 23.04 0.5123850 15.02 17.00 0.99 1173.07 0.50 457.72 1.08 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.08 308.41 0.706451 23.04 0.5123850 15.02 17.00 0.99 1172.34 0.50 458.35 1.09 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.09 308.04 0.706451 23.04 0.5123850 15.02 17.00 0.99 1171.61 0.50 458.99 1.10 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.11 307.68 0.706451 23.05 0.5123850 15.03 17.00 0.99 1170.89 0.50 459.63 1.12 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.12 307.32 0.706451 23.05 0.5123850 15.03 17.00 0.99 1170.16 0.50 460.29 1.13 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.13 306.98 0.706451 23.05 0.5123850 15.03 17.00 0.99 1169.43 0.50 460.94 1.14 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.14 306.65 0.706451 23.06 0.5123850 15.03 17.00 0.99 1168.70 0.50 461.59 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.15 306.34 0.706451 23.06 0.5123850 15.03 17.00 0.99 1167.97 0.50 462.23 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.16 306.04 0.706451 23.07 0.5123850 15.04 17.00 0.99 1167.24 0.51 462.87 1.16 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 305.76 0.706451 23.07 0.5123850 15.04 17.00 0.99 1166.51 0.51 463.51 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 305.48 0.706451 23.07 0.5123850 15.04 17.00 0.99 1165.79 0.51 464.14 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 305.22 0.706451 23.08 0.5123850 15.04 17.00 0.99 1165.06 0.51 464.76 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 304.96 0.706451 23.08 0.5123850 15.04 17.00 0.99 1164.33 0.51 465.38 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 304.71 0.706451 23.08 0.5123850 15.04 17.00 0.99 1163.60 0.51 466.00 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.19 304.47 0.706451 23.09 0.5123850 15.05 17.00 0.99 1162.87 0.51 466.61 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 304.22 0.706451 23.09 0.5123850 15.05 17.00 0.99 1162.14 0.51 467.23 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 303.98 0.706451 23.09 0.5123850 15.05 17.00 0.98 1161.41 0.51 467.84 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 303.74 0.706451 23.10 0.5123850 15.05 17.00 0.98 1160.69 0.51 468.45 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 303.49 0.706451 23.10 0.5123850 15.05 17.00 0.98 1159.96 0.51 469.07 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 303.24 0.706451 23.10 0.5123850 15.06 17.00 0.98 1159.23 0.51 469.70 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 302.98 0.706451 23.11 0.5123850 15.06 17.00 0.98 1158.50 0.51 470.33 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 302.71 0.706451 23.11 0.5123850 15.06 17.00 0.98 1157.77 0.51 470.98 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 302.44 0.706451 23.11 0.5123850 15.06 17.00 0.98 1157.04 0.51 471.64 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 302.15 0.706451 23.12 0.5123850 15.06 17.00 0.98 1156.31 0.51 472.31 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 301.85 0.706451 23.12 0.5123850 15.07 17.00 0.98 1155.59 0.51 473.01 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 301.54 0.706451 23.13 0.5123850 15.07 17.00 0.98 1154.86 0.51 473.73 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 301.22 0.706451 23.13 0.5123850 15.07 17.00 0.98 1154.13 0.51 474.46 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.23 300.89 0.706451 23.14 0.5123850 15.07 17.00 0.98 1153.40 0.51 475.21 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 300.55 0.706451 23.14 0.5123850 15.08 17.00 0.98 1152.67 0.51 475.97 1.23 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 300.20 0.706451 23.14 0.5123850 15.08 17.00 0.98 1151.94 0.51 476.74 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.25 299.85 0.706451 23.15 0.5123850 15.08 17.00 0.98 1151.21 0.52 477.51 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 299.50 0.706451 23.15 0.5123850 15.08 17.00 0.98 1150.49 0.52 478.28 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 299.15 0.706451 23.16 0.5123850 15.09 17.00 0.98 1149.76 0.52 479.05 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 298.80 0.706451 23.16 0.5123850 15.09 17.00 0.98 1149.03 0.52 479.81 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 298.46 0.706451 23.17 0.5123850 15.09 17.00 0.98 1148.30 0.52 480.56 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 298.11 0.706451 23.17 0.5123850 15.09 17.00 0.98 1147.57 0.52 481.30 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 297.77 0.706451 23.18 0.5123850 15.10 17.00 0.97 1146.84 0.52 482.03 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 297.43 0.706451 23.18 0.5123850 15.10 17.00 0.97 1146.11 0.52 482.76 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.29 297.08 0.706451 23.19 0.5123850 15.10 17.00 0.97 1145.39 0.52 483.48 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.74 0.706451 23.19 0.5123850 15.10 17.00 0.97 1144.66 0.52 484.19 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.40 0.706451 23.20 0.5123850 15.11 17.00 0.97 1143.93 0.52 484.90 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.05 0.706451 23.20 0.5123850 15.11 17.00 0.97 1143.20 0.52 485.60 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 295.70 0.706451 23.21 0.5123850 15.11 17.00 0.97 1142.47 0.52 486.30 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 295.35 0.706451 23.21 0.5123850 15.12 17.00 0.97 1141.74 0.52 486.99 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 295.00 0.706451 23.22 0.5123850 15.12 17.00 0.97 1141.01 0.52 487.68 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 294.64 0.706451 23.23 0.5123850 15.12 17.00 0.97 1140.29 0.52 488.37 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 294.27 0.706451 23.23 0.5123850 15.13 17.00 0.97 1139.56 0.52 489.06 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.91 0.706451 23.24 0.5123850 15.13 17.00 0.97 1138.83 0.52 489.76 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.53 0.706451 23.24 0.5123850 15.13 17.00 0.97 1138.10 0.52 490.45 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.15 0.706451 23.25 0.5123850 15.13 17.00 0.97 1137.37 0.52 491.14 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 292.77 0.706451 23.25 0.5123850 15.14 17.00 0.97 1136.64 0.52 491.83 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 292.38 0.706451 23.26 0.5123850 15.14 17.00 0.97 1135.91 0.53 492.52 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 291.98 0.706451 23.27 0.5123850 15.14 17.00 0.97 1135.19 0.53 493.22 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 291.58 0.706451 23.27 0.5123850 15.15 17.00 0.97 1134.46 0.53 493.91 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 291.17 0.706451 23.28 0.5123850 15.15 17.00 0.97 1133.73 0.53 494.61 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 290.75 0.706451 23.29 0.5123850 15.16 17.00 0.97 1133.00 0.53 495.31 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 290.33 0.706451 23.29 0.5123850 15.16 17.00 0.96 1132.27 0.53 496.01 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.90 0.706451 23.30 0.5123850 15.16 17.00 0.96 1131.54 0.53 496.71 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.46 0.706451 23.31 0.5123850 15.17 17.00 0.96 1130.81 0.53 497.42 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.01 0.706451 23.31 0.5123850 15.17 17.00 0.96 1130.09 0.53 498.12 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 288.56 0.706451 23.32 0.5123850 15.17 17.00 0.96 1129.36 0.53 498.83 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 288.10 0.706451 23.33 0.5123850 15.18 17.00 0.96 1128.63 0.53 499.55 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 287.64 0.706451 23.34 0.5123850 15.18 17.00 0.96 1127.90 0.53 500.26 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 287.16 0.706451 23.34 0.5123850 15.19 17.00 0.96 1127.17 0.53 500.98 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 286.68 0.706451 23.35 0.5123850 15.19 17.00 0.96 1126.44 0.53 501.70 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 286.19 0.706451 23.36 0.5123850 15.20 17.00 0.96 1125.71 0.53 502.42 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 285.69 0.706451 23.37 0.5123850 15.20 17.00 0.96 1124.99 0.53 503.15 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 285.19 0.706451 23.38 0.5123850 15.20 17.00 0.96 1124.26 0.53 503.87 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 284.67 0.706451 23.39 0.5123850 15.21 17.00 0.96 1123.53 0.53 504.61 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 284.15 0.706451 23.39 0.5123850 15.21 17.00 0.96 1122.80 0.53 505.34 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 283.62 0.706451 23.40 0.5123850 15.22 17.00 0.96 1122.07 0.53 506.08 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.05 5.80 0.97 0.30 283.08 0.706451 23.41 0.5123850 15.22 17.00 0.96 1121.34 0.54 506.82 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 282.54 0.706451 23.42 0.5123850 15.23 17.00 0.96 1120.61 0.54 507.56 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 281.98 0.706451 23.43 0.5123850 15.23 17.00 0.96 1119.88 0.54 508.30 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 281.41 0.706451 23.44 0.5123850 15.24 17.00 0.96 1119.16 0.54 509.05 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 280.84 0.706451 23.45 0.5123850 15.24 17.00 0.96 1118.43 0.54 509.80 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 280.26 0.706451 23.46 0.5123850 15.25 17.00 0.95 1117.70 0.54 510.56 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 279.66 0.706451 23.47 0.5123850 15.25 17.00 0.95 1116.97 0.54 511.32 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 279.06 0.706451 23.48 0.5123850 15.26 17.00 0.95 1116.24 0.54 512.08 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 278.45 0.706451 23.49 0.5123850 15.27 17.00 0.95 1115.51 0.54 512.85 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 277.83 0.706451 23.50 0.5123850 15.27 17.00

136 0.95 1114.78 0.54 513.61 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 277.20 0.706451 23.51 0.5123850 15.28 17.00 0.95 1114.06 0.54 514.39 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 276.56 0.706451 23.52 0.5123850 15.28 17.00 0.95 1113.33 0.54 515.16 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 275.91 0.706451 23.53 0.5123850 15.29 17.00 0.95 1112.60 0.54 515.94 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 275.25 0.706451 23.54 0.5123850 15.29 17.00 0.95 1111.87 0.54 516.73 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 274.58 0.706451 23.55 0.5123850 15.30 17.00 0.95 1111.14 0.54 517.51 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 273.90 0.706451 23.57 0.5123850 15.31 17.00 0.95 1110.41 0.54 518.30 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 273.21 0.706451 23.58 0.5123850 15.31 17.00 0.95 1109.68 0.54 519.10 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 272.50 0.706451 23.59 0.5123850 15.32 17.00 0.95 1108.96 0.54 519.90 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 271.79 0.706451 23.60 0.5123850 15.33 17.00 0.95 1108.23 0.54 520.70 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 271.07 0.706451 23.62 0.5123850 15.33 17.00 0.95 1107.50 0.55 521.50 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 270.34 0.706451 23.63 0.5123850 15.34 17.00 0.95 1106.77 0.55 522.31 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 269.59 0.706451 23.64 0.5123850 15.35 17.00 0.95 1106.04 0.55 523.13 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 268.84 0.706451 23.65 0.5123850 15.35 17.00 0.95 1105.31 0.55 523.95 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 268.07 0.706451 23.67 0.5123850 15.36 17.00 0.95 1104.58 0.55 524.77 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 267.29 0.706451 23.68 0.5123850 15.37 17.00 0.95 1103.86 0.55 525.60 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 266.50 0.706451 23.70 0.5123850 15.38 17.00 0.94 1103.13 0.55 526.43 1.24 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 265.70 0.706451 23.71 0.5123850 15.38 17.00 0.94 1102.40 0.55 527.27 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 264.89 0.706451 23.72 0.5123850 15.39 17.00 0.94 1101.67 0.55 528.11 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 264.06 0.706451 23.74 0.5123850 15.40 17.00 0.94 1100.94 0.55 528.95 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 263.23 0.706451 23.75 0.5123850 15.41 17.00 0.94 1100.21 0.55 529.80 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 262.38 0.706451 23.77 0.5123850 15.42 17.00 0.94 1099.48 0.55 530.66 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 261.52 0.706451 23.79 0.5123850 15.43 17.00 0.94 1098.76 0.55 531.52 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 260.65 0.706451 23.80 0.5123850 15.43 17.00 0.94 1098.03 0.55 532.38 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 259.76 0.706451 23.82 0.5123850 15.44 17.00 0.94 1097.30 0.55 533.25 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 258.86 0.706451 23.83 0.5123850 15.45 17.00 0.94 1096.57 0.55 534.12 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 257.95 0.706451 23.85 0.5123850 15.46 17.00 0.94 1095.84 0.55 535.00 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 257.03 0.706451 23.87 0.5123850 15.47 17.00 0.94 1095.11 0.56 535.89 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 256.10 0.706451 23.89 0.5123850 15.48 17.00 0.94 1094.38 0.56 536.78 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 255.15 0.706451 23.90 0.5123850 15.49 17.00 0.94 1093.66 0.56 537.67 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 254.19 0.706451 23.92 0.5123850 15.50 17.00 0.94 1092.93 0.56 538.57 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 253.22 0.706451 23.94 0.5123850 15.51 17.00 0.94 1092.20 0.56 539.48 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 252.23 0.706451 23.96 0.5123850 15.52 17.00 0.94 1091.47 0.56 540.39 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 251.23 0.706451 23.98 0.5123850 15.53 17.00 0.94 1090.74 0.56 541.30 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.10 5.80 0.93 0.30 250.22 0.706451 24.00 0.5123850 15.54 17.00 0.94 1090.01 0.56 542.22 1.21 0.00 0.00 0.00 0.92 0.09 0.00 0.10 5.80 0.92 0.30 249.19 0.706451 24.02 0.5123850 15.55 17.00 0.94 1089.28 0.56 543.15 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 248.15 0.706451 24.04 0.5123850 15.56 17.00 0.93 1088.56 0.56 544.09 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 247.10 0.706451 24.06 0.5123850 15.57 17.00 0.93 1087.83 0.56 545.02 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 246.03 0.706451 24.08 0.5123850 15.58 17.00 0.93 1087.10 0.56 545.97 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 244.96 0.706451 24.10 0.5123850 15.59 17.00 0.93 1086.37 0.56 546.92 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 243.86 0.706451 24.12 0.5123850 15.61 17.00 0.93 1085.64 0.56 547.88 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 242.76 0.706451 24.14 0.5123850 15.62 17.00 0.93 1084.91 0.56 548.84 1.20 0.00 0.00 0.00 0.92 0.11 0.00 0.11 5.80 0.92 0.30 241.63 0.706451 24.16 0.5123850 15.63 17.00 0.93 1084.18 0.56 549.81 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 240.50 0.706451 24.19 0.5123850 15.64 17.00 0.93 1083.46 0.57 550.78 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 239.35 0.706451 24.21 0.5123850 15.66 17.00 0.93 1082.73 0.57 551.77 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 238.19 0.706451 24.23 0.5123850 15.67 17.00 0.93 1082.00 0.57 552.75 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 237.01 0.706451 24.26 0.5123850 15.68 17.00 0.93 1081.27 0.57 553.75 1.19 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 235.82 0.706451 24.28 0.5123849 15.69 17.00 0.93 1080.54 0.57 554.75 1.18 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 234.62 0.706451 24.31 0.5123849 15.71 17.00 0.93 1079.81 0.57 555.76 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.12 5.80 0.90 0.30 233.40 0.706451 24.33 0.5123849 15.72 17.00 0.93 1079.08 0.57 556.77 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 232.17 0.706451 24.36 0.5123849 15.73 17.00 0.93 1078.36 0.57 557.79 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 230.92 0.706451 24.39 0.5123849 15.75 17.00 0.93 1077.63 0.57 558.82 1.18 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 229.66 0.706451 24.41 0.5123849 15.76 17.00 0.93 1076.90 0.57 559.86 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 228.39 0.706451 24.44 0.5123849 15.78 17.00 0.93 1076.17 0.57 560.90 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 227.10 0.706451 24.47 0.5123849 15.79 17.00 0.93 1075.44 0.57 561.95 1.17 0.00 0.00 0.00 0.89 0.13 0.00 0.14 5.80 0.89 0.30 225.80 0.706451 24.49 0.5123849 15.81 17.00 0.93 1074.71 0.57 563.00 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 224.48 0.706451 24.52 0.5123849 15.82 17.00 0.92 1073.98 0.57 564.07 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 223.15 0.706451 24.55 0.5123849 15.84 17.00 0.92 1073.26 0.58 565.14 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 221.81 0.706451 24.58 0.5123849 15.85 17.00 0.92 1072.53 0.58 566.22 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.15 5.80 0.89 0.30 220.45 0.706451 24.61 0.5123849 15.87 17.00 0.92 1071.80 0.58 567.30 1.16 0.00 0.00 0.00 0.89 0.15 0.00 0.15 5.80 0.89 0.30 219.08 0.706451 24.64 0.5123849 15.89 17.00 0.92 1071.07 0.58 568.39 1.16 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 217.69 0.706451 24.67 0.5123849 15.90 17.00 0.92 1070.34 0.58 569.49 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 216.29 0.706451 24.71 0.5123849 15.92 17.00 0.92 1069.61 0.58 570.60 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.16 5.80 0.88 0.30 214.88 0.706451 24.74 0.5123849 15.94 17.00 0.92 1068.88 0.58 571.72 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 213.45 0.706451 24.77 0.5123849 15.96 17.00 0.92 1068.16 0.58 572.84 1.15 0.00 0.00 0.00 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0.18 0.00 0.18 5.80 0.86 0.30 200.01 0.706451 25.10 0.5123849 16.13 17.00 0.92 1061.60 0.59 583.31 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.19 5.80 0.86 0.30 198.45 0.706451 25.14 0.5123849 16.15 17.00 0.92 1060.87 0.59 584.52 1.12 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 196.88 0.706451 25.18 0.5123849 16.17 17.00 0.92 1060.14 0.59 585.73 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 195.30 0.706451 25.22 0.5123849 16.19 17.00 0.91 1059.41 0.59 586.95 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 193.70 0.706451 25.26 0.5123849 16.22 17.00 0.91 1058.68 0.59 588.18 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 192.09 0.706451 25.30 0.5123849 16.24 17.00 0.91 1057.96 0.59 589.42 1.11 0.00 0.00 0.00 0.85 0.20 0.00 0.20 5.80 0.85 0.30 190.47 0.706451 25.34 0.5123848 16.26 17.00 0.91 1057.23 0.59 590.67 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.20 5.80 0.84 0.30 188.84 0.706451 25.39 0.5123848 16.29 17.00 0.91 1056.50 0.59 591.92 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.21 5.80 0.84 0.30 187.20 0.706451 25.43 0.5123848 16.31 17.00 0.91 1055.77 0.59 593.19 1.10 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 185.55 0.706451 25.48 0.5123848 16.33 17.00 0.91 1055.04 0.60 594.46 1.09 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 183.89 0.706451 25.52 0.5123848 16.36 17.00 0.91 1054.31 0.60 595.74 1.09 0.00 0.00 0.00 0.83 0.21 0.00 0.22 5.80 0.83 0.30 182.21 0.706451 25.57 0.5123848 16.38 17.00 0.91 1053.58 0.60 597.03 1.09 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 180.53 0.706451 25.62 0.5123848 16.41 17.00 0.91 1052.86 0.60 598.33 1.08 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 178.84 0.706451 25.67 0.5123848 16.43 17.00 0.91 1052.13 0.60 599.64 1.08 0.00 0.00 0.00 0.82 0.22 0.00 0.23 5.80 0.82 0.30 177.13 0.706451 25.71 0.5123848 16.46 17.00 0.91 1051.40 0.60 600.96 1.08 0.00 0.00 0.00 0.82 0.23 0.00 0.23 5.80 0.82 0.30 175.42 0.706451 25.76 0.5123848 16.49 17.00 0.91 1050.67 0.60 602.29 1.07 0.00 0.00 0.00 0.82 0.23 0.00 0.24 5.80 0.82 0.30 173.70 0.706451 25.82 0.5123848 16.51 17.00 0.91 1049.94 0.60 603.62 1.07 0.00 0.00 0.00 0.82 0.24 0.00 0.24 5.80 0.82 0.30 171.97 0.706451 25.87 0.5123848 16.54 17.00 0.91 1049.21 0.60 604.97 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.24 5.80 0.81 0.30 170.23 0.706451 25.92 0.5123848 16.57 17.00 0.91 1048.48 0.60 606.32 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.25 5.80 0.81 0.30 168.48 0.706451 25.97 0.5123848 16.60 17.00 0.91 1047.76 0.60 607.68 1.06 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 166.72 0.706452 26.03 0.5123847 16.63 17.00 0.91 1047.03 0.61 609.06 1.05 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 164.96 0.706452 26.08 0.5123847 16.66 17.00 0.91 1046.30 0.61 610.44 1.05 0.00 0.00 0.00 0.80 0.25 0.00 0.26 5.80 0.80 0.30 163.19 0.706452 26.14 0.5123847 16.69 17.00 0.91 1045.57 0.61 611.83 1.05 0.00 0.00 0.00 0.80 0.26 0.00 0.26 5.80 0.80 0.30 161.41 0.706452 26.20 0.5123847 16.72 17.00 0.90 1044.84 0.61 613.23 1.04 0.00 0.00 0.00 0.80 0.26 0.00 0.27 5.80 0.80 0.30 159.62 0.706452 26.26 0.5123847 16.75 17.00 0.90 1044.11 0.61 614.63 1.04 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 157.83 0.706452 26.32 0.5123847 16.78 17.00 0.90 1043.38 0.61 616.05 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 156.04 0.706452 26.38 0.5123847 16.81 17.00 0.90 1042.66 0.61 617.48 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.28 5.80 0.79 0.30 154.23 0.706452 26.44 0.5123847 16.84 17.00 0.90 1041.93 0.61 618.92 1.03 0.00 0.00 0.00 0.78 0.28 0.00 0.28 5.80 0.78 0.30 152.43 0.706452 26.50 0.5123846 16.88 17.00 0.90 1041.20 0.61 620.36 1.02 0.00 0.00 0.00 0.78 0.28 0.00 0.29 5.80 0.78 0.30 150.61 0.706452 26.56 0.5123846 16.91 17.00 0.90 1040.47 0.61 621.82 1.02 0.00 0.00 0.00 0.78 0.29 0.00 0.29 5.80 0.78 0.30 148.80 0.706452 26.63 0.5123846 16.95 17.00 0.90 1039.74 0.62 623.28 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.29 5.80 0.77 0.30 146.98 0.706452 26.69 0.5123846 16.98 17.00 0.90 1039.01 0.62 624.75 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.30 5.80 0.77 0.30 145.15 0.706452 26.76 0.5123846 17.02 17.00 0.90 1038.28 0.62 626.23 1.01 0.00 0.00 0.00 0.77 0.30 0.00 0.30 5.80 0.77 0.30 143.33 0.706452 26.83 0.5123845 17.05 17.00 0.90 1037.56 0.62 627.72 1.00 0.00 0.00 0.00 0.76 0.30 0.00 0.31 5.80 0.76 0.30 141.50 0.706452 26.90 0.5123845 17.09 17.00 0.90 1036.83 0.62 629.22 1.00 0.00 0.00 0.00 0.76 0.31 0.00 0.31 5.80 0.76 0.30 139.67 0.706452 26.97 0.5123845 17.13 17.00 0.90 1036.10 0.62 630.73 0.99 0.00 0.00 0.00 0.76 0.31 0.00 0.32 5.80 0.76 0.30 137.83 0.706452 27.04 0.5123845 17.16 17.00 0.90 1035.37 0.62 632.25 0.99 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 136.00 0.706452 27.11 0.5123845 17.20 17.00 0.90 1034.64 0.62 633.78 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 134.17 0.706452 27.19 0.5123844 17.24 17.00 0.90 1033.91 0.62 635.31 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.33 5.80 0.75 0.30 132.33 0.706453 27.26 0.5123844 17.28 17.00 0.90 1033.18 0.62 636.86 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.33 5.80 0.74 0.30 130.50 0.706453 27.34 0.5123844 17.32 17.00 0.90 1032.46 0.63 638.41 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.34 5.80 0.74 0.30 128.66 0.706453 27.42 0.5123843 17.36 17.00 0.90 1031.73 0.63 639.97 0.97 0.00 0.00 0.00 0.74 0.34 0.00 0.34 5.80 0.74 0.30 126.83 0.706453 27.50 0.5123843 17.40 17.00 0.90 1031.00 0.63 641.54 0.96 0.00 0.00 0.00 0.73 0.34 0.00 0.35 5.80 0.73 0.30 125.00 0.706453 27.58 0.5123843 17.45 17.00 0.89 1030.27 0.63 643.12 0.96 0.00 0.00 0.00 0.73 0.35 0.00 0.35 5.80 0.73 0.30 123.17 0.706453 27.66 0.5123842 17.49 17.00 0.89 1029.54 0.63 644.71 0.95 0.00 0.00 0.00 0.73 0.35 0.00 0.36 5.80 0.73 0.30 121.34 0.706453 27.74 0.5123842 17.53 17.00 0.89 1028.81 0.63 646.31 0.95 0.00 0.00 0.00 0.72 0.36 0.00 0.36 5.80 0.72 0.30 119.52 0.706453 27.83 0.5123842 17.58 17.00

137 0.89 1028.08 0.63 647.91 0.94 0.00 0.00 0.00 0.72 0.36 0.00 0.37 5.80 0.72 0.30 117.70 0.706454 27.91 0.5123841 17.62 17.00 0.89 1027.36 0.63 649.52 0.94 0.00 0.00 0.00 0.72 0.37 0.00 0.37 5.80 0.72 0.30 115.88 0.706454 28.00 0.5123841 17.67 17.00 0.89 1026.63 0.63 651.15 0.93 0.00 0.00 0.00 0.71 0.37 0.00 0.38 5.80 0.71 0.30 114.07 0.706454 28.09 0.5123840 17.71 17.00 0.89 1025.90 0.64 652.77 0.93 0.00 0.00 0.00 0.71 0.38 0.00 0.38 5.80 0.71 0.30 112.26 0.706454 28.18 0.5123840 17.76 17.00 0.89 1025.17 0.64 654.41 0.92 0.00 0.00 0.00 0.70 0.38 0.00 0.39 5.80 0.70 0.30 110.46 0.706454 28.27 0.5123839 17.81 17.00 0.89 1024.44 0.64 656.06 0.92 0.00 0.00 0.00 0.70 0.39 0.00 0.39 5.80 0.70 0.30 108.67 0.706454 28.36 0.5123839 17.86 17.00 0.89 1023.71 0.64 657.71 0.91 0.00 0.00 0.00 0.70 0.39 0.00 0.40 5.80 0.70 0.30 106.88 0.706455 28.46 0.5123838 17.91 17.00 0.89 1022.98 0.64 659.37 0.91 0.00 0.00 0.00 0.69 0.40 0.00 0.40 5.80 0.69 0.30 105.09 0.706455 28.55 0.5123838 17.96 17.00 0.89 1022.26 0.64 661.04 0.90 0.00 0.00 0.00 0.69 0.40 0.00 0.41 5.80 0.69 0.30 103.32 0.706455 28.65 0.5123837 18.01 17.00 0.89 1021.53 0.64 662.71 0.90 0.00 0.00 0.00 0.68 0.41 0.00 0.41 5.80 0.68 0.30 101.55 0.706456 28.75 0.5123836 18.06 17.00 0.89 1020.80 0.64 664.40 0.89 0.00 0.00 0.00 0.68 0.41 0.00 0.42 5.80 0.68 0.30 99.80 0.706456 28.85 0.5123836 18.11 17.00 0.89 1020.07 0.64 666.09 0.89 0.00 0.00 0.00 0.68 0.42 0.00 0.42 5.80 0.68 0.30 98.05 0.706456 28.96 0.5123835 18.17 17.00 0.89 1019.34 0.65 667.78 0.88 0.00 0.00 0.00 0.67 0.42 0.00 0.43 5.80 0.67 0.30 96.31 0.706457 29.06 0.5123834 18.22 17.00 0.89 1018.61 0.65 669.49 0.88 0.00 0.00 0.00 0.67 0.43 0.00 0.43 5.80 0.67 0.30 94.58 0.706457 29.17 0.5123833 18.28 17.00 0.89 1017.88 0.65 671.20 0.87 0.00 0.00 0.00 0.66 0.43 0.00 0.44 5.80 0.66 0.30 92.86 0.706458 29.28 0.5123832 18.33 17.00 0.89 1017.16 0.65 672.92 0.87 0.00 0.00 0.00 0.66 0.44 0.00 0.44 5.80 0.66 0.30 91.15 0.706458 29.39 0.5123831 18.39 17.00 0.89 1016.43 0.65 674.64 0.86 0.00 0.00 0.00 0.66 0.44 0.00 0.45 5.80 0.66 0.30 89.45 0.706459 29.50 0.5123830 18.45 17.00 0.88 1015.70 0.65 676.37 0.85 0.00 0.00 0.00 0.65 0.45 0.00 0.45 5.80 0.65 0.30 87.77 0.706459 29.61 0.5123829 18.51 17.00 0.88 1014.97 0.65 678.11 0.85 0.00 0.00 0.00 0.65 0.46 0.00 0.46 5.80 0.65 0.30 86.09 0.706460 29.73 0.5123828 18.57 17.00 0.88 1014.24 0.65 679.85 0.84 0.00 0.00 0.00 0.64 0.46 0.00 0.46 5.80 0.64 0.30 84.43 0.706460 29.84 0.5123827 18.63 17.00 0.88 1013.51 0.66 681.61 0.84 0.00 0.00 0.00 0.64 0.47 0.00 0.47 5.80 0.64 0.30 82.79 0.706461 29.96 0.5123826 18.69 17.00 0.88 1012.78 0.66 683.37 0.83 0.00 0.00 0.00 0.63 0.47 0.00 0.48 5.80 0.63 0.30 81.15 0.706462 30.08 0.5123824 18.75 17.00 0.88 1012.06 0.66 685.13 0.83 0.00 0.00 0.00 0.63 0.48 0.00 0.48 5.80 0.63 0.30 79.53 0.706463 30.21 0.5123823 18.81 17.00 0.88 1011.33 0.66 686.91 0.82 0.00 0.00 0.00 0.63 0.48 0.00 0.49 5.80 0.63 0.30 77.92 0.706464 30.33 0.5123822 18.88 17.00 0.88 1010.60 0.66 688.70 0.82 0.00 0.00 0.00 0.62 0.49 0.00 0.49 5.80 0.62 0.30 76.33 0.706465 30.46 0.5123820 18.94 17.01 0.88 1009.87 0.66 690.50 0.81 0.00 0.00 0.00 0.62 0.49 0.00 0.50 5.79 0.62 0.30 74.75 0.706466 30.59 0.5123818 19.01 17.01 0.88 1009.14 0.66 692.33 0.80 0.00 0.00 0.00 0.61 0.50 0.00 0.50 5.79 0.61 0.30 73.19 0.706467 30.72 0.5123817 19.08 17.01 0.88 1008.41 0.66 694.18 0.80 0.00 0.00 0.00 0.61 0.51 0.00 0.51 5.79 0.61 0.30 71.64 0.706468 30.85 0.5123815 19.14 17.01 0.88 1007.68 0.67 696.07 0.79 0.00 0.00 0.00 0.60 0.51 0.00 0.52 5.79 0.60 0.30 70.11 0.706470 30.99 0.5123813 19.21 17.01 0.88 1006.96 0.67 698.02 0.79 0.00 0.00 0.00 0.60 0.52 0.00 0.52 5.79 0.60 0.30 68.60 0.706471 31.13 0.5123810 19.28 17.01 0.88 1006.23 0.67 700.03 0.78 0.00 0.00 0.00 0.60 0.52 0.01 0.53 5.79 0.60 0.30 67.10 0.706473 31.27 0.5123808 19.35 17.01 0.88 1005.50 0.67 702.15 0.78 0.00 0.00 0.00 0.59 0.53 0.01 0.54 5.79 0.59 0.30 65.61 0.706475 31.41 0.5123805 19.43 17.01 0.88 1004.77 0.67 704.39 0.77 0.00 0.00 0.00 0.59 0.54 0.01 0.54 5.79 0.59 0.31 64.14 0.706478 31.55 0.5123802 19.50 17.01 0.88 1004.04 0.67 706.81 0.77 0.00 0.00 0.00 0.58 0.54 0.01 0.55 5.79 0.58 0.31 62.69 0.706481 31.70 0.5123798 19.57 17.01 0.88 1003.31 0.67 709.43 0.77 0.00 0.00 0.00 0.58 0.55 0.01 0.56 5.79 0.58 0.31 61.25 0.706484 31.85 0.5123794 19.65 17.01 0.88 1002.58 0.68 712.30 0.76 0.00 0.00 0.00 0.57 0.55 0.01 0.57 5.79 0.57 0.32 59.83 0.706488 32.01 0.5123790 19.73 17.01 0.88 1001.86 0.68 715.46 0.76 0.00 0.00 0.00 0.57 0.56 0.02 0.58 5.79 0.57 0.33 58.43 0.706493 32.16 0.5123784 19.81 17.01 0.87 1001.13 0.68 718.93 0.76 0.00 0.00 0.00 0.56 0.56 0.02 0.59 5.79 0.56 0.33 57.04 0.706500 32.33 0.5123777 19.89 17.01 0.87 1000.40 0.68 722.71 0.76 0.00 0.00 0.00 0.56 0.57 0.02 0.60 5.79 0.56 0.34 55.67 0.706507 32.49 0.5123769 19.97 17.01 0.87 999.67 0.69 726.77 0.76 0.00 0.00 0.00 0.55 0.58 0.03 0.61 5.78 0.55 0.35 54.32 0.706517 32.66 0.5123759 20.05 17.02 0.87 998.94 0.69 731.08 0.76 0.00 0.00 0.00 0.55 0.58 0.04 0.62 5.78 0.55 0.37 52.98 0.706529 32.83 0.5123747 20.13 17.02 0.87 998.21 0.69 735.55 0.76 0.00 0.00 0.00 0.55 0.59 0.04 0.63 5.78 0.55 0.38 51.67 0.706543 33.01 0.5123734 20.22 17.02 0.87 997.48 0.70 740.10 0.76 0.00 0.00 0.00 0.54 0.60 0.05 0.64 5.78 0.54 0.39 50.38 0.706560 33.20 0.5123718 20.30 17.02 0.87 996.75 0.70 744.65 0.76 0.00 0.00 0.00 0.54 0.60 0.05 0.66 5.77 0.54 0.40 49.12 0.706579 33.38 0.5123700 20.39 17.03 0.87 996.03 0.70 749.12 0.77 0.00 0.00 0.00 0.53 0.61 0.06 0.67 5.77 0.53 0.42 47.88 0.706602 33.57 0.5123681 20.48 17.03 0.87 995.30 0.70 753.45 0.77 0.00 0.01 0.01 0.53 0.62 0.06 0.68 5.77 0.53 0.43 46.66 0.706627 33.77 0.5123659 20.57 17.03 0.87 994.57 0.71 757.58 0.76 0.00 0.01 0.01 0.52 0.62 0.07 0.69 5.76 0.52 0.44 45.47 0.706656 33.97 0.5123636 20.66 17.04 0.87 993.84 0.71 761.49 0.76 0.00 0.01 0.01 0.52 0.63 0.07 0.70 5.76 0.52 0.45 44.31 0.706686 34.17 0.5123611 20.75 17.04 0.87 993.11 0.71 765.18 0.76 0.00 0.01 0.01 0.51 0.64 0.08 0.71 5.75 0.51 0.46 43.17 0.706720 34.38 0.5123586 20.84 17.05 0.87 992.38 0.71 768.63 0.76 0.00 0.01 0.01 0.51 0.64 0.08 0.72 5.75 0.51 0.46 42.06 0.706755 34.59 0.5123559 20.93 17.05 0.87 991.65 0.72 771.87 0.76 0.00 0.01 0.01 0.50 0.65 0.08 0.73 5.74 0.50 0.47 40.97 0.706793 34.81 0.5123531 21.03 17.05 0.87 990.93 0.72 774.91 0.75 0.01 0.01 0.01 0.50 0.66 0.09 0.74 5.73 0.50 0.48 39.90 0.706834 35.03 0.5123503 21.12 17.06 0.87 990.20 0.72 777.77 0.75 0.01 0.01 0.01 0.49 0.66 0.09 0.75 5.73 0.49 0.48 38.86 0.706877 35.25 0.5123474 21.22 17.07 0.87 989.47 0.72 780.47 0.75 0.01 0.01 0.01 0.49 0.67 0.09 0.76 5.72 0.49 0.48 37.84 0.706922 35.47 0.5123444 21.32 17.07 0.87 988.74 0.72 783.04 0.74 0.01 0.01 0.01 0.49 0.68 0.09 0.77 5.72 0.49 0.49 36.84 0.706970 35.70 0.5123413 21.42 17.08 0.87 988.01 0.73 785.49 0.74 0.01 0.01 0.01 0.48 0.68 0.09 0.77 5.71 0.48 0.49 35.87 0.707021 35.93 0.5123382 21.52 17.08 0.87 987.28 0.73 787.83 0.73 0.01 0.01 0.01 0.48 0.69 0.09 0.78 5.70 0.48 0.49 34.92 0.707075 36.17 0.5123350 21.62 17.09 0.86 986.55 0.73 790.09 0.73 0.01 0.01 0.01 0.47 0.70 0.09 0.79 5.70 0.47 0.49 33.99 0.707132 36.40 0.5123317 21.72 17.09 0.86 985.83 0.73 792.28 0.72 0.01 0.02 0.02 0.47 0.70 0.09 0.80 5.69 0.47 0.49 33.08 0.707193 36.65 0.5123282 21.82 17.10 0.86 985.10 0.73 794.40 0.72 0.01 0.02 0.02 0.46 0.71 0.09 0.81 5.68 0.46 0.49 32.20 0.707259 36.89 0.5123247 21.93 17.11 0.86 984.37 0.73 796.46 0.71 0.01 0.02 0.02 0.46 0.72 0.09 0.81 5.67 0.46 0.50 31.34 0.707329 37.14 0.5123211 22.03 17.11 0.86 983.64 0.74 798.48 0.70 0.01 0.02 0.02 0.45 0.72 0.10 0.82 5.67 0.45 0.50 30.51 0.707403 37.40 0.5123173 22.14 17.12 0.86 982.91 0.74 800.46 0.70 0.01 0.02 0.02 0.45 0.73 0.10 0.83 5.66 0.45 0.50 29.69 0.707483 37.66 0.5123134 22.24 17.13 0.86 982.18 0.74 802.40 0.69 0.01 0.02 0.02 0.44 0.74 0.10 0.83 5.65 0.44 0.50 28.90 0.707569 37.92 0.5123093 22.35 17.13 0.86 981.45 0.74 804.31 0.69 0.01 0.02 0.02 0.44 0.75 0.10 0.84 5.64 0.44 0.50 28.13 0.707661 38.19 0.5123051 22.46 17.14 0.86 980.73 0.74 806.19 0.68 0.01 0.02 0.02 0.44 0.75 0.10 0.85 5.63 0.44 0.50 27.39 0.707760 38.46 0.5123007 22.57 17.15 0.86 980.00 0.74 808.04 0.68 0.01 0.02 0.02 0.43 0.76 0.10 0.85 5.62 0.43 0.50 26.66 0.707866 38.74 0.5122962 22.68 17.16 0.86 979.27 0.74 809.87 0.67 0.01 0.03 0.03 0.43 0.77 0.10 0.86 5.61 0.43 0.50 25.96 0.707979 39.02 0.5122915 22.79 17.17 0.86 978.54 0.74 811.67 0.67 0.01 0.03 0.03 0.42 0.77 0.10 0.87 5.60 0.42 0.50 25.28 0.708100 39.30 0.5122866 22.90 17.17 0.86 977.81 0.75 813.45 0.66 0.02 0.03 0.03 0.42 0.78 0.10 0.88 5.59 0.42 0.50 24.63 0.708230 39.59 0.5122816 23.02 17.18 0.86 977.08 0.75 815.21 0.66 0.02 0.03 0.03 0.41 0.79 0.10 0.88 5.57 0.41 0.50 23.99 0.708368 39.89 0.5122764 23.13 17.19 0.86 976.35 0.75 816.95 0.65 0.02 0.03 0.03 0.41 0.79 0.10 0.89 5.56 0.41 0.50 23.38 0.708516 40.19 0.5122710 23.25 17.20 0.86 975.63 0.75 818.67 0.65 0.02 0.03 0.03 0.40 0.80 0.10 0.90 5.55 0.40 0.50 22.79 0.708673 40.49 0.5122654 23.36 17.21 0.86 974.90 0.75 820.36 0.64 0.02 0.03 0.03 0.40 0.81 0.10 0.90 5.53 0.40 0.50 22.23 0.708840 40.80 0.5122596 23.48 17.23 0.86 974.17 0.75 822.04 0.64 0.02 0.04 0.04 0.39 0.81 0.10 0.91 5.52 0.39 0.50 21.68 0.709018 41.11 0.5122537 23.59 17.24 0.86 973.44 0.75 823.70 0.63 0.02 0.04 0.04 0.39 0.82 0.10 0.92 5.51 0.39 0.50 21.16 0.709206 41.43 0.5122476 23.71 17.25 0.86 972.71 0.75 825.33 0.63 0.02 0.04 0.04 0.39 0.83 0.10 0.92 5.49 0.39 0.50 20.66 0.709405 41.75 0.5122413 23.83 17.26 0.85 971.98 0.75 826.95 0.62 0.02 0.04 0.04 0.38 0.83 0.10 0.93 5.47 0.38 0.50 20.18 0.709616 42.08 0.5122348 23.94 17.27 0.85 971.25 0.76 828.55 0.62 0.02 0.04 0.04 0.38 0.84 0.10 0.94 5.46 0.38 0.50 19.72 0.709837 42.41 0.5122282 24.06 17.29 0.85 970.53 0.76 830.13 0.61 0.02 0.05 0.05 0.37 0.85 0.10 0.94 5.44 0.37 0.50 19.28 0.710071 42.74 0.5122214 24.18 17.30 0.85 969.80 0.76 831.69 0.61 0.03 0.05 0.05 0.37 0.85 0.10 0.95 5.42 0.37 0.50 18.86 0.710316 43.08 0.5122144 24.30 17.31 0.85 969.07 0.76 833.22 0.60 0.03 0.05 0.05 0.36 0.86 0.10 0.95 5.40 0.36 0.50 18.47 0.710572 43.42 0.5122072 24.41 17.33 0.85 968.34 0.76 834.75 0.60 0.03 0.05 0.05 0.36 0.86 0.10 0.96 5.38 0.36 0.50 18.09 0.710840 43.77 0.5121999 24.53 17.34 0.85 967.61 0.76 836.25 0.60 0.03 0.05 0.05 0.36 0.87 0.10 0.97 5.36 0.36 0.50 17.73 0.711119 44.12 0.5121925 24.65 17.36 0.85 966.88 0.76 837.73 0.59 0.03 0.06 0.06 0.35 0.88 0.10 0.97 5.34 0.35 0.50 17.39 0.711409 44.47 0.5121848 24.77 17.37 0.85 966.15 0.76 839.19 0.59 0.03 0.06 0.06 0.35 0.88 0.10 0.98 5.32 0.35 0.50 17.08 0.711711 44.83 0.5121771 24.88 17.39 0.85 965.43 0.76 840.63 0.58 0.03 0.06 0.06 0.34 0.89 0.10 0.99 5.30 0.34 0.50 16.78 0.712022 45.19 0.5121691 25.00 17.40 0.85 964.70 0.77 842.06 0.58 0.03 0.06 0.06 0.34 0.90 0.10 0.99 5.28 0.34 0.50 16.50 0.712344 45.55 0.5121611 25.12 17.42 0.85 963.97 0.77 843.46 0.58 0.04 0.07 0.07 0.33 0.90 0.10 1.00 5.26 0.33 0.50 16.23 0.712674 45.91 0.5121529 25.23 17.44 0.85 963.24 0.77 844.85 0.57 0.04 0.07 0.07 0.33 0.91 0.10 1.00 5.23 0.33 0.50 15.99 0.713014 46.28 0.5121446 25.35 17.45 0.85 962.51 0.77 846.22 0.57 0.04 0.07 0.07 0.33 0.91 0.10 1.01 5.21 0.33 0.50 15.76 0.713361 46.65 0.5121362 25.47 17.47 0.85 961.78 0.77 847.56 0.57 0.04 0.08 0.08 0.32 0.92 0.10 1.02 5.19 0.32 0.50 15.55 0.713716 47.02 0.5121276 25.58 17.49 0.85 961.05 0.77 848.90 0.56 0.04 0.08 0.08 0.32 0.93 0.10 1.02 5.16 0.32 0.50 15.35 0.714077 47.40 0.5121190 25.69 17.51 0.85 960.33 0.77 850.21 0.56 0.04 0.08 0.08 0.31 0.93 0.10 1.03 5.14 0.31 0.50 15.18 0.714444 47.77 0.5121102 25.81 17.53 0.85 959.60 0.77 851.50 0.56 0.05 0.08 0.08 0.31 0.94 0.10 1.03 5.11 0.31 0.50 15.01 0.714816 48.15 0.5121014 25.92 17.54 0.85 958.87 0.77 852.78 0.55 0.05 0.09 0.09 0.31 0.94 0.10 1.04 5.08 0.31 0.50 14.87 0.715191 48.53 0.5120925 26.03 17.56 0.85 958.14 0.77 854.03 0.55 0.05 0.09 0.09 0.30 0.95 0.10 1.05 5.06 0.30 0.50 14.73 0.715569 48.91 0.5120835 26.14 17.58 0.84 957.41 0.77 855.27 0.55 0.05 0.09 0.09 0.30 0.96 0.10 1.05 5.03 0.30 0.50 14.62 0.715949 49.29 0.5120744 26.25 17.60 0.84 956.68 0.78 856.50 0.55 0.05 0.10 0.10 0.30 0.96 0.10 1.06 5.00 0.30 0.50 14.51 0.716329 49.67 0.5120653 26.36 17.62 0.84 955.95 0.78 857.70 0.54 0.05 0.10 0.10 0.29 0.97 0.10 1.06 4.97 0.29 0.50 14.42 0.716709 50.06 0.5120561 26.46 17.64 0.84 955.23 0.78 858.89 0.54 0.06 0.10 0.10 0.29 0.97 0.10 1.07 4.94 0.29 0.50 14.34 0.717088 50.44 0.5120469 26.57 17.66 0.84 954.50 0.78 860.06 0.54 0.06 0.11 0.11 0.28 0.98 0.10 1.08 4.91 0.28 0.50 14.28 0.717465 50.82 0.5120377 26.67 17.68 0.84 953.77 0.78 861.22 0.54 0.06 0.11 0.11 0.28 0.98 0.10 1.08 4.88 0.28 0.50 14.23 0.717839 51.20 0.5120284 26.77 17.70 0.84 953.04 0.78 862.36 0.53 0.06 0.11 0.11 0.28 0.99 0.10 1.09 4.85 0.28 0.50 14.19 0.718209 51.58 0.5120191 26.87 17.72 0.84 952.31 0.78 863.48 0.53 0.06 0.12 0.12 0.27 1.00 0.10 1.09 4.82 0.27 0.50 14.16 0.718574 51.96 0.5120097 26.97 17.75 0.84 951.58 0.78 864.59 0.53 0.07 0.12 0.12 0.27 1.00 0.10 1.10 4.79 0.27 0.50 14.14 0.718934 52.34 0.5120004 27.07 17.77 0.84 950.85 0.78 865.68 0.53 0.07 0.12 0.12 0.27 1.01 0.10 1.10 4.76 0.27 0.50 14.14 0.719288 52.71 0.5119910 27.17 17.79 0.84 950.13 0.78 866.75 0.53 0.07 0.13 0.13 0.26 1.01 0.10 1.11 4.73 0.26 0.50 14.14 0.719635 53.09 0.5119816 27.26 17.81 0.84 949.40 0.78 867.82 0.53 0.07 0.13 0.13 0.26 1.02 0.10 1.11 4.70 0.26 0.50 14.16 0.719975 53.46 0.5119723 27.35 17.83 0.84 948.67 0.78 868.86 0.52 0.07 0.13 0.13 0.25 1.02 0.10 1.12 4.67 0.25 0.50 14.18 0.720308 53.83 0.5119630 27.44 17.85 0.84 947.94 0.78 869.89 0.52 0.08 0.14 0.14 0.25 1.03 0.10 1.12 4.64 0.25 0.50 14.21 0.720632 54.20 0.5119536 27.53 17.88 0.84 947.21 0.79 870.91 0.52 0.08 0.14 0.14 0.25 1.03 0.10 1.13 4.60 0.25 0.50 14.26 0.720948 54.57 0.5119443 27.62 17.90 0.84 946.48 0.79 871.92 0.52 0.08 0.15 0.15 0.24 1.04 0.10 1.13 4.57 0.24 0.50 14.31 0.721254 54.93 0.5119350 27.70 17.92

138 0.84 945.75 0.79 872.91 0.52 0.08 0.15 0.15 0.24 1.04 0.10 1.14 4.54 0.24 0.50 14.36 0.721552 55.29 0.5119258 27.78 17.94 0.84 945.03 0.79 873.88 0.52 0.08 0.15 0.15 0.24 1.05 0.10 1.14 4.51 0.24 0.50 14.43 0.721841 55.65 0.5119166 27.86 17.97 0.84 944.30 0.79 874.85 0.52 0.09 0.16 0.16 0.23 1.05 0.10 1.15 4.47 0.23 0.50 14.51 0.722120 56.00 0.5119074 27.94 17.99 0.84 943.57 0.79 875.80 0.52 0.09 0.16 0.16 0.23 1.06 0.10 1.15 4.44 0.23 0.50 14.59 0.722390 56.35 0.5118983 28.02 18.01 0.83 942.84 0.79 876.73 0.52 0.09 0.17 0.17 0.23 1.06 0.10 1.16 4.41 0.23 0.50 14.68 0.722651 56.69 0.5118892 28.09 18.03 0.83 942.11 0.79 877.66 0.51 0.09 0.17 0.17 0.22 1.07 0.10 1.16 4.37 0.22 0.50 14.77 0.722902 57.04 0.5118802 28.17 18.06 0.83 941.38 0.79 878.57 0.51 0.09 0.17 0.17 0.22 1.07 0.10 1.17 4.34 0.22 0.50 14.87 0.723144 57.37 0.5118712 28.24 18.08 0.83 940.65 0.79 879.47 0.51 0.10 0.18 0.18 0.22 1.08 0.10 1.17 4.31 0.22 0.50 14.98 0.723377 57.71 0.5118623 28.30 18.10 0.83 939.93 0.79 880.36 0.51 0.10 0.18 0.18 0.21 1.08 0.10 1.18 4.27 0.21 0.50 15.09 0.723601 58.03 0.5118535 28.37 18.12 0.83 939.20 0.79 881.24 0.51 0.10 0.19 0.19 0.21 1.09 0.10 1.18 4.24 0.21 0.50 15.21 0.723816 58.36 0.5118447 28.43 18.15 0.83 938.47 0.79 882.11 0.51 0.10 0.19 0.19 0.21 1.09 0.10 1.19 4.21 0.21 0.50 15.34 0.724022 58.68 0.5118359 28.49 18.17 0.83 937.74 0.79 882.96 0.51 0.11 0.20 0.20 0.21 1.10 0.10 1.19 4.18 0.21 0.50 15.47 0.724220 58.99 0.5118273 28.55 18.19 0.83 937.01 0.79 883.81 0.51 0.11 0.20 0.20 0.20 1.10 0.10 1.20 4.14 0.20 0.50 15.60 0.724409 59.30 0.5118187 28.61 18.21 0.83 936.28 0.79 884.64 0.51 0.11 0.20 0.20 0.20 1.10 0.10 1.20 4.11 0.20 0.50 15.74 0.724591 59.60 0.5118102 28.66 18.24 0.83 935.55 0.80 885.47 0.51 0.11 0.21 0.21 0.20 1.11 0.10 1.21 4.08 0.20 0.50 15.89 0.724764 59.90 0.5118018 28.71 18.26 0.83 934.83 0.80 886.28 0.51 0.12 0.21 0.21 0.19 1.11 0.10 1.21 4.04 0.19 0.50 16.04 0.724930 60.19 0.5117934 28.76 18.28 0.83 934.10 0.80 887.08 0.51 0.12 0.22 0.22 0.19 1.12 0.10 1.21 4.01 0.19 0.50 16.19 0.725089 60.48 0.5117851 28.81 18.30 0.83 933.37 0.80 887.88 0.51 0.12 0.22 0.22 0.19 1.12 0.10 1.22 3.98 0.19 0.50 16.35 0.725241 60.76 0.5117770 28.86 18.32 0.83 932.64 0.80 888.66 0.51 0.12 0.23 0.23 0.19 1.13 0.10 1.22 3.95 0.19 0.50 16.51 0.725386 61.03 0.5117688 28.90 18.35 0.83 931.91 0.80 889.44 0.51 0.13 0.23 0.23 0.18 1.13 0.10 1.23 3.91 0.18 0.50 16.68 0.725524 61.30 0.5117608 28.94 18.37 0.83 931.18 0.80 890.21 0.51 0.13 0.24 0.24 0.18 1.13 0.10 1.23 3.88 0.18 0.50 16.84 0.725656 61.57 0.5117529 28.98 18.39 0.83 930.45 0.80 890.96 0.51 0.13 0.24 0.24 0.18 1.14 0.10 1.23 3.85 0.18 0.50 17.02 0.725782 61.83 0.5117450 29.01 18.41 0.83 929.73 0.80 891.71 0.51 0.13 0.24 0.24 0.17 1.14 0.10 1.24 3.82 0.17 0.50 17.19 0.725902 62.08 0.5117372 29.05 18.43 0.83 929.00 0.80 892.45 0.51 0.14 0.25 0.25 0.17 1.15 0.10 1.24 3.79 0.17 0.50 17.37 0.726017 62.32 0.5117295 29.08 18.45 0.82 928.27 0.80 893.18 0.52 0.14 0.25 0.25 0.17 1.15 0.10 1.25 3.76 0.17 0.50 17.55 0.726127 62.56 0.5117219 29.11 18.48 0.82 927.54 0.80 893.91 0.52 0.14 0.26 0.26 0.17 1.15 0.10 1.25 3.73 0.17 0.50 17.74 0.726231 62.80 0.5117144 29.14 18.50 0.82 926.81 0.80 894.62 0.52 0.14 0.26 0.26 0.16 1.16 0.10 1.25 3.69 0.16 0.50 17.92 0.726330 63.02 0.5117069 29.17 18.52 0.82 926.08 0.80 895.33 0.52 0.15 0.27 0.27 0.16 1.16 0.10 1.26 3.66 0.16 0.50 18.11 0.726425 63.25 0.5116996 29.19 18.54 0.82 925.35 0.80 896.03 0.52 0.15 0.27 0.27 0.16 1.17 0.10 1.26 3.63 0.16 0.50 18.31 0.726516 63.46 0.5116923 29.21 18.56 0.82 924.63 0.80 896.73 0.52 0.15 0.28 0.28 0.16 1.17 0.10 1.27 3.60 0.16 0.50 18.50 0.726602 63.67 0.5116851 29.23 18.58 0.82 923.90 0.80 897.41 0.52 0.15 0.28 0.28 0.15 1.17 0.10 1.27 3.57 0.15 0.50 18.70 0.726684 63.88 0.5116780 29.25 18.60 0.82 923.17 0.80 898.09 0.52 0.16 0.29 0.29 0.15 1.18 0.10 1.27 3.54 0.15 0.50 18.90 0.726763 64.07 0.5116710 29.26 18.62 0.82 922.44 0.80 898.76 0.52 0.16 0.29 0.29 0.15 1.18 0.10 1.28 3.51 0.15 0.50 19.11 0.726838 64.26 0.5116640 29.28 18.64 0.82 921.71 0.80 899.43 0.52 0.16 0.30 0.30 0.15 1.18 0.10 1.28 3.49 0.15 0.50 19.31 0.726909 64.45 0.5116572 29.29 18.66 0.82 920.98 0.81 900.09 0.53 0.16 0.30 0.30 0.14 1.19 0.10 1.28 3.46 0.14 0.50 19.52 0.726977 64.63 0.5116504 29.30 18.68 0.82 920.25 0.81 900.74 0.53 0.17 0.31 0.31 0.14 1.19 0.10 1.29 3.43 0.14 0.50 19.73 0.727042 64.80 0.5116437 29.31 18.70 0.82 919.53 0.81 901.38 0.53 0.17 0.31 0.31 0.14 1.19 0.10 1.29 3.40 0.14 0.50 19.94 0.727104 64.97 0.5116371 29.32 18.72 0.82 918.80 0.81 902.02 0.53 0.17 0.32 0.32 0.14 1.20 0.10 1.29 3.37 0.14 0.50 20.16 0.727163 65.13 0.5116306 29.32 18.74 0.82 918.07 0.81 902.66 0.53 0.17 0.32 0.32 0.14 1.20 0.10 1.30 3.34 0.14 0.50 20.37 0.727220 65.29 0.5116242 29.32 18.76 0.82 917.34 0.81 903.28 0.53 0.18 0.33 0.33 0.13 1.20 0.10 1.30 3.32 0.13 0.50 20.59 0.727274 65.44 0.5116178 29.33 18.78 0.82 916.61 0.81 903.91 0.54 0.18 0.33 0.33 0.13 1.21 0.10 1.30 3.29 0.13 0.50 20.81 0.727325 65.58 0.5116115 29.33 18.80 0.82 915.88 0.81 904.52 0.54 0.18 0.34 0.34 0.13 1.21 0.10 1.31 3.26 0.13 0.50 21.03 0.727374 65.72 0.5116053 29.32 18.82 0.82 915.15 0.81 905.13 0.54 0.18 0.34 0.34 0.13 1.21 0.10 1.31 3.24 0.13 0.50 21.26 0.727421 65.85 0.5115992 29.32 18.84 0.82 914.43 0.81 905.74 0.54 0.19 0.35 0.35 0.13 1.22 0.10 1.31 3.21 0.13 0.50 21.48 0.727466 65.98 0.5115932 29.32 18.85 0.81 913.70 0.81 906.34 0.54 0.19 0.35 0.35 0.12 1.22 0.10 1.32 3.18 0.12 0.50 21.71 0.727509 66.10 0.5115872 29.31 18.87 0.81 912.97 0.81 906.93 0.54 0.19 0.35 0.35 0.12 1.22 0.10 1.32 3.16 0.12 0.50 21.94 0.727550 66.22 0.5115813 29.30 18.89 0.81 912.24 0.81 907.52 0.55 0.19 0.36 0.36 0.12 1.22 0.10 1.32 3.13 0.12 0.50 22.17 0.727589 66.33 0.5115755 29.29 18.91 0.81 911.51 0.81 908.11 0.55 0.20 0.36 0.36 0.12 1.23 0.10 1.32 3.11 0.12 0.50 22.41 0.727626 66.43 0.5115698 29.28 18.93 0.81 910.78 0.81 908.69 0.55 0.20 0.37 0.37 0.12 1.23 0.10 1.33 3.08 0.12 0.50 22.64 0.727662 66.53 0.5115641 29.27 18.94 0.81 910.05 0.81 909.27 0.55 0.20 0.37 0.37 0.11 1.23 0.10 1.33 3.06 0.11 0.50 22.88 0.727696 66.63 0.5115585 29.25 18.96

139 EC-RAXFC Results - Melts Page MODEL C - Junction Butte

Equilibration Parameters tlm 1184 degC 18O/16O in magma 5.8 Magma a 450 Mro 0.5 Element Name Sr Nd Pb Teq Norm 0.828 tmo 1184 degC 18O/16O in assimilant 0.5 Magma b -11 Episodic Recharge Magma: conc. 312 23 15 Teq deg C 933.36848 tla 1129 degC 18O/16O in recharge 5.8 Assimilant a 400 Episode deltaMri Tm,i mr,i d,i bulk Dmo 4 0.4 0.5 Mm 0.789011608 tao 450 degC Oxygen conc magma 0.47 Assimilant b -11 1 0.2 1000 0.3 2 enthalpy 0 0 0 Mao 1.496315856 tlr 1184 degC Oxygen conc assimilant 0.5 Recharge Magma a 450 2 0.2 1175 0.3 2 Assimilant: conc. 436 38 15 Ma* 0.50669112 tro 1184 degC Oxygen conc recharge 0.47 Recharge Magma b -11 3 0.1 1155 0.3 2 bulk Dao 6 0.6 0.7 Mc 1.121043362 ts 750 degC enthalpy 0 0 0 Men 0.09663615 cpm 1100 J/kg K Recharge: conc. 300 23 15 Ms 1.217679512 cpa 1000 J/kg K bulk Dro 4 0.4 0.5 fa 0.338625777 cpr 1100 J/kg K enthalpy 0 0 0 fm 0.188213659 hm 400000 J/kg Isotope Name 87Sr/86Sr 143Nd/144Nd 206Pb/204Pb fr 0.188213659 ha 350000 J/kg ratio in magma 0.706451 0.512385 17 hr 400000 J/kg ratio in assimilant 0.728666 0.510803 21.9 X 1 Normalized fraction of Wallrock melt ratio in recharge 0.706451 0.512385 17 mixed into Magma body

Norm T T magma Norm T T assim magma (deg C) assim (deg C) Mm fa Ma* X Ma* fm Mc Men Ms delO18 fr Mr Sr 87Sr/86Sr Nd 143Nd/144Nd Pb 206Pb/204Pb

1.00 1184.00 0.50 450.00 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 312.00 0.706451 23.00 0.512385 15.00 17.00 1.00 1183.27 0.50 450.57 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.86 0.706451 23.00 0.512385 15.00 17.00 1.00 1182.54 0.50 451.15 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.72 0.706451 23.00 0.512385 15.00 17.00 1.00 1181.81 0.50 451.73 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.57 0.706451 23.01 0.512385 15.00 17.00 1.00 1181.09 0.50 452.31 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.41 0.706451 23.01 0.512385 15.00 17.00 1.00 1180.36 0.50 452.89 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 311.24 0.706451 23.01 0.512385 15.01 17.00 1.00 1179.63 0.50 453.48 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 311.06 0.706451 23.01 0.512385 15.01 17.00 1.00 1178.90 0.50 454.08 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 310.85 0.706451 23.02 0.512385 15.01 17.00 1.00 1178.17 0.50 454.70 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 310.63 0.706451 23.02 0.512385 15.01 17.00 1.00 1177.44 0.50 455.32 1.02 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.02 310.38 0.706451 23.02 0.512385 15.01 17.00 1.00 1176.71 0.50 455.97 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.03 310.11 0.706451 23.02 0.512385 15.01 17.00 0.99 1175.99 0.50 456.63 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.04 309.81 0.706451 23.03 0.512385 15.01 17.00 0.99 1175.26 0.50 457.32 1.04 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.05 309.49 0.706451 23.03 0.512385 15.02 17.00 0.99 1174.53 0.50 458.04 1.05 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.06 309.14 0.706451 23.03 0.512385 15.02 17.00 0.99 1173.80 0.50 458.77 1.07 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.07 308.78 0.706451 23.04 0.512385 15.02 17.00 0.99 1173.07 0.50 459.53 1.08 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.08 308.41 0.706451 23.04 0.512385 15.02 17.00 0.99 1172.34 0.50 460.31 1.09 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.09 308.04 0.706451 23.04 0.512385 15.02 17.00 0.99 1171.61 0.50 461.10 1.10 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.11 307.68 0.706451 23.05 0.512385 15.03 17.00 0.99 1170.89 0.50 461.90 1.12 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.12 307.32 0.706451 23.05 0.512385 15.03 17.00 0.99 1170.16 0.50 462.70 1.13 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.13 306.98 0.706451 23.05 0.512385 15.03 17.00 0.99 1169.43 0.51 463.51 1.14 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.14 306.65 0.706451 23.06 0.512385 15.03 17.00 0.99 1168.70 0.51 464.31 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.15 306.34 0.706451 23.06 0.512385 15.03 17.00 0.99 1167.97 0.51 465.11 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.16 306.04 0.706451 23.07 0.512385 15.04 17.00 0.99 1167.24 0.51 465.90 1.16 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 305.76 0.706451 23.07 0.512385 15.04 17.00 0.99 1166.51 0.51 466.68 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 305.48 0.706451 23.07 0.512385 15.04 17.00 0.99 1165.79 0.51 467.46 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 305.22 0.706451 23.08 0.512385 15.04 17.00 0.99 1165.06 0.51 468.23 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 304.96 0.706451 23.08 0.512385 15.04 17.00 0.99 1164.33 0.51 469.00 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 304.71 0.706451 23.08 0.512385 15.04 17.00 0.99 1163.60 0.51 469.76 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.19 304.47 0.706451 23.09 0.512385 15.05 17.00 0.99 1162.87 0.51 470.52 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 304.22 0.706451 23.09 0.512385 15.05 17.00 0.99 1162.14 0.51 471.27 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 303.98 0.706451 23.09 0.512385 15.05 17.00 0.98 1161.41 0.51 472.03 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 303.74 0.706451 23.10 0.512385 15.05 17.00 0.98 1160.69 0.51 472.79 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 303.49 0.706451 23.10 0.512385 15.05 17.00 0.98 1159.96 0.51 473.55 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 303.24 0.706451 23.10 0.512385 15.06 17.00 0.98 1159.23 0.51 474.32 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 302.98 0.706451 23.11 0.512385 15.06 17.00 0.98 1158.50 0.51 475.11 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 302.71 0.706451 23.11 0.512385 15.06 17.00 0.98 1157.77 0.51 475.90 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 302.44 0.706451 23.11 0.512385 15.06 17.00 0.98 1157.04 0.51 476.72 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 302.15 0.706451 23.12 0.512385 15.06 17.00 0.98 1156.31 0.52 477.56 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 301.85 0.706451 23.12 0.512385 15.07 17.00 0.98 1155.59 0.52 478.42 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 301.54 0.706451 23.13 0.512385 15.07 17.00 0.98 1154.86 0.52 479.30 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 301.22 0.706451 23.13 0.512385 15.07 17.00 0.98 1154.13 0.52 480.21 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.23 300.89 0.706451 23.14 0.512385 15.07 17.00 0.98 1153.40 0.52 481.14 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 300.55 0.706451 23.14 0.512385 15.08 17.00 0.98 1152.67 0.52 482.08 1.23 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 300.20 0.706451 23.14 0.512385 15.08 17.00 0.98 1151.94 0.52 483.02 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.25 299.85 0.706451 23.15 0.512385 15.08 17.00 0.98 1151.21 0.52 483.98 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 299.50 0.706451 23.15 0.512385 15.08 17.00 0.98 1150.49 0.52 484.93 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 299.15 0.706451 23.16 0.512385 15.09 17.00 0.98 1149.76 0.52 485.87 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 298.80 0.706451 23.16 0.512385 15.09 17.00 0.98 1149.03 0.52 486.81 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 298.46 0.706451 23.17 0.512385 15.09 17.00 0.98 1148.30 0.52 487.74 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 298.11 0.706451 23.17 0.512385 15.09 17.00 0.98 1147.57 0.52 488.66 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 297.77 0.706451 23.18 0.512385 15.10 17.00 0.97 1146.84 0.52 489.56 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 297.43 0.706451 23.18 0.512385 15.10 17.00 0.97 1146.11 0.52 490.46 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.29 297.08 0.706451 23.19 0.512385 15.10 17.00 0.97 1145.39 0.52 491.35 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.74 0.706451 23.19 0.512385 15.10 17.00 0.97 1144.66 0.53 492.22 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.40 0.706451 23.20 0.512385 15.11 17.00 0.97 1143.93 0.53 493.10 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 296.05 0.706451 23.20 0.512385 15.11 17.00 0.97 1143.20 0.53 493.96 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 295.70 0.706451 23.21 0.512385 15.11 17.00 0.97 1142.47 0.53 494.82 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 295.35 0.706451 23.21 0.512385 15.12 17.00 0.97 1141.74 0.53 495.68 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 295.00 0.706451 23.22 0.512385 15.12 17.00 0.97 1141.01 0.53 496.54 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 294.64 0.706451 23.23 0.512385 15.12 17.00 0.97 1140.29 0.53 497.39 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 294.27 0.706451 23.23 0.512385 15.13 17.00 0.97 1139.56 0.53 498.25 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.91 0.706451 23.24 0.512385 15.13 17.00 0.97 1138.83 0.53 499.10 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.53 0.706451 23.24 0.512385 15.13 17.00 0.97 1138.10 0.53 499.95 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 293.15 0.706451 23.25 0.512385 15.13 17.00 0.97 1137.37 0.53 500.80 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 292.77 0.706451 23.25 0.512385 15.14 17.00 0.97 1136.64 0.53 501.66 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 292.38 0.706451 23.26 0.512385 15.14 17.00 0.97 1135.91 0.53 502.51 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 291.98 0.706451 23.27 0.512385 15.14 17.00 0.97 1135.19 0.53 503.37 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 291.58 0.706451 23.27 0.512385 15.15 17.00 0.97 1134.46 0.53 504.23 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 291.17 0.706451 23.28 0.512385 15.15 17.00 0.97 1133.73 0.53 505.09 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 290.75 0.706451 23.29 0.512385 15.16 17.00 0.97 1133.00 0.53 505.95 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 290.33 0.706451 23.29 0.512385 15.16 17.00 0.96 1132.27 0.54 506.82 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.90 0.706451 23.30 0.512385 15.16 17.00 0.96 1131.54 0.54 507.69 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.46 0.706451 23.31 0.512385 15.17 17.00 0.96 1130.81 0.54 508.56 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 289.01 0.706451 23.31 0.512385 15.17 17.00 0.96 1130.09 0.54 509.43 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 288.56 0.706451 23.32 0.512385 15.17 17.00 0.96 1129.36 0.54 510.31 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 288.10 0.706451 23.33 0.512385 15.18 17.00 0.96 1128.63 0.54 511.19 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 287.64 0.706451 23.34 0.512385 15.18 17.00 0.96 1127.90 0.54 512.07 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 287.16 0.706451 23.34 0.512385 15.19 17.00 0.96 1127.17 0.54 512.96 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 286.68 0.706451 23.35 0.512385 15.19 17.00 0.96 1126.44 0.54 513.85 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 286.19 0.706451 23.36 0.512385 15.20 17.00 0.96 1125.71 0.54 514.74 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 285.69 0.706451 23.37 0.512385 15.20 17.00 0.96 1124.99 0.54 515.64 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 285.19 0.706451 23.38 0.512385 15.20 17.00 0.96 1124.26 0.54 516.54 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 284.67 0.706451 23.39 0.512385 15.21 17.00 0.96 1123.53 0.54 517.44 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 284.15 0.706451 23.39 0.512385 15.21 17.00 0.96 1122.80 0.54 518.34 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 283.62 0.706451 23.40 0.512385 15.22 17.00 0.96 1122.07 0.54 519.25 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.05 5.80 0.97 0.30 283.08 0.706451 23.41 0.512385 15.22 17.00 0.96 1121.34 0.54 520.17 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 282.54 0.706451 23.42 0.512385 15.23 17.00 0.96 1120.61 0.55 521.08 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 281.98 0.706451 23.43 0.512385 15.23 17.00 0.96 1119.88 0.55 522.01 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 281.41 0.706451 23.44 0.512385 15.24 17.00 0.96 1119.16 0.55 522.93 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 280.84 0.706451 23.45 0.512385 15.24 17.00 0.96 1118.43 0.55 523.86 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 280.26 0.706451 23.46 0.512385 15.25 17.00 0.95 1117.70 0.55 524.79 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 279.66 0.706451 23.47 0.512385 15.25 17.00 0.95 1116.97 0.55 525.73 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 279.06 0.706451 23.48 0.512385 15.26 17.00 0.95 1116.24 0.55 526.67 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 278.45 0.706451 23.49 0.512385 15.27 17.00

140 0.95 1115.51 0.55 527.61 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 277.83 0.706451 23.50 0.512385 15.27 17.00 0.95 1114.78 0.55 528.56 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 277.20 0.706451 23.51 0.512385 15.28 17.00 0.95 1114.06 0.55 529.52 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 276.56 0.706451 23.52 0.512385 15.28 17.00 0.95 1113.33 0.55 530.48 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 275.91 0.706451 23.53 0.512385 15.29 17.00 0.95 1112.60 0.55 531.44 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 275.25 0.706451 23.54 0.512385 15.29 17.00 0.95 1111.87 0.55 532.41 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 274.58 0.706451 23.55 0.512385 15.30 17.00 0.95 1111.14 0.55 533.38 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 273.90 0.706451 23.57 0.512385 15.31 17.00 0.95 1110.41 0.55 534.35 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 273.21 0.706451 23.58 0.512385 15.31 17.00 0.95 1109.68 0.55 535.34 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 272.50 0.706451 23.59 0.512385 15.32 17.00 0.95 1108.96 0.56 536.32 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 271.79 0.706451 23.60 0.512385 15.33 17.00 0.95 1108.23 0.56 537.31 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 271.07 0.706451 23.62 0.512385 15.33 17.00 0.95 1107.50 0.56 538.31 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 270.34 0.706451 23.63 0.512385 15.34 17.00 0.95 1106.77 0.56 539.31 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 269.59 0.706451 23.64 0.512385 15.35 17.00 0.95 1106.04 0.56 540.31 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 268.84 0.706451 23.65 0.512385 15.35 17.00 0.95 1105.31 0.56 541.33 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 268.07 0.706451 23.67 0.512385 15.36 17.00 0.95 1104.58 0.56 542.34 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 267.29 0.706451 23.68 0.512385 15.37 17.00 0.95 1103.86 0.56 543.36 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 266.50 0.706451 23.70 0.512385 15.38 17.00 0.94 1103.13 0.56 544.39 1.24 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 265.70 0.706451 23.71 0.512385 15.38 17.00 0.94 1102.40 0.56 545.42 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 264.89 0.706451 23.72 0.512385 15.39 17.00 0.94 1101.67 0.56 546.46 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 264.06 0.706451 23.74 0.512385 15.40 17.00 0.94 1100.94 0.56 547.51 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 263.23 0.706451 23.75 0.512385 15.41 17.00 0.94 1100.21 0.56 548.55 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 262.38 0.706451 23.77 0.512385 15.42 17.00 0.94 1099.48 0.56 549.61 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 261.52 0.706451 23.79 0.512385 15.43 17.00 0.94 1098.76 0.57 550.67 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 260.65 0.706451 23.80 0.512385 15.43 17.00 0.94 1098.03 0.57 551.74 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 259.76 0.706451 23.82 0.512385 15.44 17.00 0.94 1097.30 0.57 552.81 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 258.86 0.706451 23.83 0.512385 15.45 17.00 0.94 1096.57 0.57 553.89 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 257.95 0.706451 23.85 0.512385 15.46 17.00 0.94 1095.84 0.57 554.98 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 257.03 0.706451 23.87 0.512385 15.47 17.00 0.94 1095.11 0.57 556.07 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 256.10 0.706451 23.89 0.512385 15.48 17.00 0.94 1094.38 0.57 557.17 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 255.15 0.706451 23.90 0.512385 15.49 17.00 0.94 1093.66 0.57 558.27 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 254.19 0.706451 23.92 0.512385 15.50 17.00 0.94 1092.93 0.57 559.38 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 253.22 0.706451 23.94 0.512385 15.51 17.00 0.94 1092.20 0.57 560.50 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 252.23 0.706451 23.96 0.512385 15.52 17.00 0.94 1091.47 0.57 561.63 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 251.23 0.706451 23.98 0.512385 15.53 17.00 0.94 1090.74 0.57 562.76 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.10 5.80 0.93 0.30 250.22 0.706451 24.00 0.512385 15.54 17.00 0.94 1090.01 0.57 563.90 1.21 0.00 0.00 0.00 0.92 0.09 0.00 0.10 5.80 0.92 0.30 249.19 0.706451 24.02 0.512385 15.55 17.00 0.94 1089.28 0.58 565.04 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 248.15 0.706451 24.04 0.512385 15.56 17.00 0.93 1088.56 0.58 566.19 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 247.10 0.706451 24.06 0.512385 15.57 17.00 0.93 1087.83 0.58 567.35 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 246.03 0.706451 24.08 0.512385 15.58 17.00 0.93 1087.10 0.58 568.52 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 244.95 0.706451 24.10 0.512385 15.59 17.00 0.93 1086.37 0.58 569.69 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 243.86 0.706451 24.12 0.512385 15.61 17.00 0.93 1085.64 0.58 570.88 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 242.75 0.706451 24.14 0.512385 15.62 17.00 0.93 1084.91 0.58 572.06 1.20 0.00 0.00 0.00 0.92 0.11 0.00 0.11 5.80 0.92 0.30 241.63 0.706451 24.17 0.512385 15.63 17.00 0.93 1084.18 0.58 573.26 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 240.50 0.706451 24.19 0.512385 15.64 17.00 0.93 1083.46 0.58 574.47 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 239.35 0.706451 24.21 0.512385 15.66 17.00 0.93 1082.73 0.58 575.68 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 238.19 0.706451 24.23 0.512385 15.67 17.00 0.93 1082.00 0.58 576.90 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 237.01 0.706451 24.26 0.512385 15.68 17.00 0.93 1081.27 0.58 578.13 1.19 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 235.82 0.706451 24.28 0.512385 15.69 17.00 0.93 1080.54 0.59 579.36 1.18 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 234.62 0.706451 24.31 0.512385 15.71 17.00 0.93 1079.81 0.59 580.61 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.12 5.80 0.90 0.30 233.40 0.706451 24.33 0.512385 15.72 17.00 0.93 1079.08 0.59 581.86 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 232.17 0.706451 24.36 0.512385 15.73 17.00 0.93 1078.36 0.59 583.12 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 230.92 0.706451 24.39 0.512385 15.75 17.00 0.93 1077.63 0.59 584.39 1.18 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 229.66 0.706451 24.41 0.512385 15.76 17.00 0.93 1076.90 0.59 585.67 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 228.39 0.706451 24.44 0.512385 15.78 17.00 0.93 1076.17 0.59 586.95 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 227.10 0.706451 24.47 0.512385 15.79 17.00 0.93 1075.44 0.59 588.25 1.17 0.00 0.00 0.00 0.89 0.13 0.00 0.14 5.80 0.89 0.30 225.80 0.706451 24.50 0.512385 15.81 17.00 0.93 1074.71 0.59 589.55 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 224.48 0.706451 24.52 0.512385 15.82 17.00 0.92 1073.98 0.59 590.87 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 223.15 0.706451 24.55 0.512385 15.84 17.00 0.92 1073.26 0.59 592.19 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 221.81 0.706451 24.58 0.512385 15.86 17.00 0.92 1072.53 0.59 593.52 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.15 5.80 0.89 0.30 220.45 0.706451 24.61 0.512385 15.87 17.00 0.92 1071.80 0.60 594.86 1.16 0.00 0.00 0.00 0.89 0.15 0.00 0.15 5.80 0.89 0.30 219.08 0.706451 24.64 0.512385 15.89 17.00 0.92 1071.07 0.60 596.21 1.16 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 217.69 0.706451 24.68 0.512385 15.90 17.00 0.92 1070.34 0.60 597.57 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 216.29 0.706451 24.71 0.512385 15.92 17.00 0.92 1069.61 0.60 598.93 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.16 5.80 0.88 0.30 214.88 0.706451 24.74 0.512385 15.94 17.00 0.92 1068.88 0.60 600.31 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 213.45 0.706451 24.77 0.512385 15.96 17.00 0.92 1068.16 0.60 601.70 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 212.01 0.706451 24.81 0.512385 15.97 17.00 0.92 1067.43 0.60 603.09 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.16 5.80 0.87 0.30 210.55 0.706451 24.84 0.512385 15.99 17.00 0.92 1066.70 0.60 604.50 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.17 5.80 0.87 0.30 209.09 0.706451 24.88 0.512385 16.01 17.00 0.92 1065.97 0.60 605.92 1.14 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 207.61 0.706451 24.91 0.512385 16.03 17.00 0.92 1065.24 0.60 607.34 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 206.11 0.706451 24.95 0.512385 16.05 17.00 0.92 1064.51 0.61 608.78 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.18 5.80 0.87 0.30 204.60 0.706451 24.98 0.512385 16.07 17.00 0.92 1063.78 0.61 610.22 1.13 0.00 0.00 0.00 0.86 0.17 0.00 0.18 5.80 0.86 0.30 203.08 0.706451 25.02 0.512385 16.09 17.00 0.92 1063.06 0.61 611.68 1.13 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 201.55 0.706451 25.06 0.512385 16.11 17.00 0.92 1062.33 0.61 613.15 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 200.00 0.706451 25.10 0.512385 16.13 17.00 0.92 1061.60 0.61 614.62 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.19 5.80 0.86 0.30 198.45 0.706451 25.14 0.512385 16.15 17.00 0.92 1060.87 0.61 616.11 1.12 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 196.87 0.706451 25.18 0.512385 16.17 17.00 0.92 1060.14 0.61 617.61 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 195.29 0.706451 25.22 0.512385 16.20 17.00 0.91 1059.41 0.61 619.11 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 193.70 0.706452 25.26 0.512385 16.22 17.00 0.91 1058.68 0.61 620.63 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 192.09 0.706452 25.30 0.512385 16.24 17.00 0.91 1057.96 0.61 622.16 1.11 0.00 0.00 0.00 0.85 0.20 0.00 0.20 5.80 0.85 0.30 190.47 0.706452 25.34 0.512385 16.26 17.00 0.91 1057.23 0.62 623.70 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.20 5.80 0.84 0.30 188.84 0.706452 25.39 0.512385 16.29 17.00 0.91 1056.50 0.62 625.25 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.21 5.80 0.84 0.30 187.20 0.706452 25.43 0.512385 16.31 17.00 0.91 1055.77 0.62 626.81 1.10 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 185.55 0.706452 25.48 0.512385 16.33 17.00 0.91 1055.04 0.62 628.38 1.09 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 183.88 0.706452 25.52 0.512385 16.36 17.00 0.91 1054.31 0.62 629.96 1.09 0.00 0.00 0.00 0.83 0.21 0.00 0.22 5.80 0.83 0.30 182.21 0.706452 25.57 0.512385 16.38 17.00 0.91 1053.58 0.62 631.55 1.09 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 180.53 0.706452 25.62 0.512385 16.41 17.00 0.91 1052.86 0.62 633.16 1.08 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 178.83 0.706452 25.67 0.512385 16.43 17.00 0.91 1052.13 0.62 634.77 1.08 0.00 0.00 0.00 0.82 0.22 0.00 0.23 5.80 0.82 0.30 177.13 0.706452 25.72 0.512385 16.46 17.00 0.91 1051.40 0.62 636.40 1.08 0.00 0.00 0.00 0.82 0.23 0.00 0.23 5.80 0.82 0.30 175.41 0.706452 25.77 0.512385 16.49 17.00 0.91 1050.67 0.63 638.03 1.07 0.00 0.00 0.00 0.82 0.23 0.00 0.24 5.80 0.82 0.30 173.69 0.706452 25.82 0.512384 16.51 17.00

141 0.91 1049.94 0.63 639.68 1.07 0.00 0.00 0.00 0.82 0.24 0.00 0.24 5.80 0.82 0.30 171.96 0.706452 25.87 0.512384 16.54 17.00 0.91 1049.21 0.63 641.34 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.24 5.80 0.81 0.30 170.22 0.706452 25.92 0.512384 16.57 17.00 0.91 1048.48 0.63 643.01 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.25 5.80 0.81 0.30 168.47 0.706452 25.98 0.512384 16.60 17.00 0.91 1047.76 0.63 644.69 1.06 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 166.71 0.706452 26.03 0.512384 16.63 17.00 0.91 1047.03 0.63 646.38 1.05 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 164.95 0.706452 26.09 0.512384 16.66 17.00 0.91 1046.30 0.63 648.09 1.05 0.00 0.00 0.00 0.80 0.25 0.00 0.26 5.80 0.80 0.30 163.18 0.706452 26.14 0.512384 16.69 17.00 0.91 1045.57 0.63 649.80 1.05 0.00 0.00 0.00 0.80 0.26 0.00 0.26 5.80 0.80 0.30 161.40 0.706453 26.20 0.512384 16.72 17.00 0.90 1044.84 0.63 651.53 1.04 0.00 0.00 0.00 0.80 0.26 0.00 0.27 5.80 0.80 0.30 159.61 0.706453 26.26 0.512384 16.75 17.00 0.90 1044.11 0.64 653.26 1.04 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 157.82 0.706453 26.32 0.512384 16.78 17.00 0.90 1043.38 0.64 655.01 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 156.03 0.706453 26.38 0.512384 16.81 17.00 0.90 1042.66 0.64 656.77 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.28 5.80 0.79 0.30 154.22 0.706453 26.44 0.512384 16.85 17.00 0.90 1041.93 0.64 658.54 1.03 0.00 0.00 0.00 0.78 0.28 0.00 0.28 5.80 0.78 0.30 152.42 0.706453 26.51 0.512384 16.88 17.00 0.90 1041.20 0.64 660.32 1.02 0.00 0.00 0.00 0.78 0.28 0.00 0.29 5.80 0.78 0.30 150.60 0.706453 26.57 0.512384 16.91 17.00 0.90 1040.47 0.64 662.11 1.02 0.00 0.00 0.00 0.78 0.29 0.00 0.29 5.80 0.78 0.30 148.79 0.706453 26.64 0.512384 16.95 17.00 0.90 1039.74 0.64 663.91 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.29 5.80 0.77 0.30 146.97 0.706454 26.70 0.512384 16.98 17.00 0.90 1039.01 0.64 665.73 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.30 5.80 0.77 0.30 145.14 0.706454 26.77 0.512384 17.02 17.00 0.90 1038.28 0.65 667.55 1.01 0.00 0.00 0.00 0.77 0.30 0.00 0.30 5.80 0.77 0.30 143.32 0.706454 26.84 0.512384 17.05 17.00 0.90 1037.56 0.65 669.39 1.00 0.00 0.00 0.00 0.76 0.30 0.00 0.31 5.80 0.76 0.30 141.49 0.706454 26.91 0.512384 17.09 17.00 0.90 1036.83 0.65 671.23 1.00 0.00 0.00 0.00 0.76 0.31 0.00 0.31 5.80 0.76 0.30 139.66 0.706454 26.98 0.512384 17.13 17.00 0.90 1036.10 0.65 673.09 0.99 0.00 0.00 0.00 0.76 0.31 0.00 0.32 5.80 0.76 0.30 137.82 0.706455 27.05 0.512384 17.16 17.00 0.90 1035.37 0.65 674.96 0.99 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 135.99 0.706455 27.12 0.512383 17.20 17.00 0.90 1034.64 0.65 676.84 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 134.15 0.706455 27.20 0.512383 17.24 17.00 0.90 1033.91 0.65 678.73 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.33 5.80 0.75 0.30 132.32 0.706456 27.27 0.512383 17.28 17.00 0.90 1033.18 0.65 680.62 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.33 5.80 0.74 0.30 130.48 0.706456 27.35 0.512383 17.32 17.00 0.90 1032.46 0.66 682.53 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.34 5.80 0.74 0.30 128.65 0.706456 27.43 0.512383 17.36 17.00 0.90 1031.73 0.66 684.45 0.97 0.00 0.00 0.00 0.74 0.34 0.00 0.34 5.80 0.74 0.30 126.81 0.706457 27.51 0.512383 17.41 17.00 0.90 1031.00 0.66 686.38 0.96 0.00 0.00 0.00 0.73 0.34 0.00 0.35 5.80 0.73 0.30 124.98 0.706457 27.59 0.512383 17.45 17.00 0.89 1030.27 0.66 688.32 0.96 0.00 0.00 0.00 0.73 0.35 0.00 0.35 5.80 0.73 0.30 123.15 0.706458 27.67 0.512383 17.49 17.00 0.89 1029.54 0.66 690.27 0.95 0.00 0.00 0.00 0.73 0.35 0.00 0.36 5.80 0.73 0.30 121.32 0.706458 27.76 0.512383 17.53 17.00 0.89 1028.81 0.66 692.23 0.95 0.00 0.00 0.00 0.72 0.36 0.00 0.36 5.80 0.72 0.30 119.50 0.706459 27.84 0.512382 17.58 17.00 0.89 1028.08 0.66 694.20 0.94 0.00 0.00 0.00 0.72 0.36 0.00 0.37 5.80 0.72 0.30 117.68 0.706459 27.93 0.512382 17.62 17.00 0.89 1027.36 0.67 696.18 0.94 0.00 0.00 0.00 0.72 0.37 0.00 0.37 5.80 0.72 0.30 115.86 0.706460 28.02 0.512382 17.67 17.00 0.89 1026.63 0.67 698.17 0.93 0.00 0.00 0.00 0.71 0.37 0.00 0.38 5.80 0.71 0.30 114.05 0.706461 28.11 0.512382 17.72 17.01 0.89 1025.90 0.67 700.17 0.93 0.00 0.00 0.00 0.71 0.38 0.00 0.38 5.80 0.71 0.30 112.24 0.706461 28.20 0.512382 17.76 17.01 0.89 1025.17 0.67 702.17 0.92 0.00 0.00 0.00 0.70 0.38 0.00 0.39 5.79 0.70 0.30 110.44 0.706462 28.29 0.512382 17.81 17.01 0.89 1024.44 0.67 704.19 0.92 0.00 0.00 0.00 0.70 0.39 0.00 0.39 5.79 0.70 0.30 108.65 0.706463 28.39 0.512381 17.86 17.01 0.89 1023.71 0.67 706.21 0.91 0.00 0.00 0.00 0.70 0.39 0.00 0.40 5.79 0.70 0.30 106.86 0.706464 28.49 0.512381 17.91 17.01 0.89 1022.98 0.67 708.24 0.91 0.00 0.00 0.00 0.69 0.40 0.00 0.40 5.79 0.69 0.30 105.08 0.706465 28.58 0.512381 17.96 17.01 0.89 1022.26 0.67 710.28 0.90 0.00 0.00 0.00 0.69 0.40 0.00 0.41 5.79 0.69 0.30 103.30 0.706466 28.68 0.512381 18.01 17.01 0.89 1021.53 0.68 712.33 0.90 0.00 0.00 0.00 0.68 0.41 0.00 0.41 5.79 0.68 0.30 101.54 0.706467 28.79 0.512380 18.06 17.01 0.89 1020.80 0.68 714.38 0.89 0.00 0.00 0.00 0.68 0.41 0.00 0.42 5.79 0.68 0.30 99.78 0.706469 28.89 0.512380 18.12 17.01 0.89 1020.07 0.68 716.44 0.89 0.00 0.00 0.00 0.68 0.42 0.00 0.42 5.79 0.68 0.30 98.03 0.706470 28.99 0.512380 18.17 17.01 0.89 1019.34 0.68 718.51 0.88 0.00 0.00 0.00 0.67 0.42 0.00 0.43 5.79 0.67 0.30 96.29 0.706472 29.10 0.512379 18.22 17.01 0.89 1018.61 0.68 720.59 0.88 0.00 0.00 0.00 0.67 0.43 0.00 0.43 5.79 0.67 0.30 94.56 0.706474 29.21 0.512379 18.28 17.01 0.89 1017.88 0.68 722.67 0.87 0.00 0.00 0.00 0.66 0.43 0.00 0.44 5.79 0.66 0.30 92.85 0.706476 29.32 0.512379 18.34 17.01 0.89 1017.16 0.68 724.76 0.87 0.00 0.00 0.00 0.66 0.44 0.00 0.44 5.79 0.66 0.30 91.14 0.706478 29.43 0.512378 18.39 17.01 0.89 1016.43 0.69 726.86 0.86 0.00 0.00 0.00 0.66 0.44 0.00 0.45 5.79 0.66 0.30 89.44 0.706480 29.55 0.512378 18.45 17.01 0.88 1015.70 0.69 728.96 0.86 0.00 0.00 0.00 0.65 0.45 0.00 0.45 5.79 0.65 0.30 87.76 0.706483 29.67 0.512377 18.51 17.01 0.88 1014.97 0.69 731.07 0.85 0.00 0.00 0.00 0.65 0.46 0.00 0.46 5.79 0.65 0.30 86.09 0.706486 29.79 0.512377 18.57 17.01 0.88 1014.24 0.69 733.18 0.85 0.00 0.00 0.00 0.64 0.46 0.00 0.46 5.79 0.64 0.30 84.43 0.706489 29.91 0.512376 18.63 17.01 0.88 1013.51 0.69 735.30 0.84 0.00 0.00 0.00 0.64 0.47 0.00 0.47 5.79 0.64 0.30 82.78 0.706492 30.03 0.512376 18.69 17.02 0.88 1012.78 0.69 737.43 0.83 0.00 0.00 0.00 0.63 0.47 0.00 0.48 5.78 0.63 0.30 81.15 0.706496 30.16 0.512375 18.76 17.02 0.88 1012.06 0.69 739.56 0.83 0.00 0.00 0.00 0.63 0.48 0.00 0.48 5.78 0.63 0.30 79.53 0.706500 30.28 0.512374 18.82 17.02 0.88 1011.33 0.70 741.71 0.82 0.00 0.00 0.00 0.63 0.48 0.00 0.49 5.78 0.63 0.30 77.93 0.706504 30.42 0.512374 18.88 17.02 0.88 1010.60 0.70 743.86 0.82 0.00 0.00 0.00 0.62 0.49 0.00 0.49 5.78 0.62 0.30 76.34 0.706509 30.55 0.512373 18.95 17.02 0.88 1009.87 0.70 746.03 0.81 0.00 0.00 0.00 0.62 0.49 0.00 0.50 5.78 0.62 0.30 74.76 0.706514 30.68 0.512372 19.02 17.02 0.88 1009.14 0.70 748.22 0.81 0.00 0.00 0.00 0.61 0.50 0.00 0.50 5.78 0.61 0.30 73.21 0.706520 30.82 0.512371 19.08 17.02 0.88 1008.41 0.70 750.44 0.80 0.00 0.00 0.00 0.61 0.51 0.00 0.51 5.78 0.61 0.30 71.66 0.706526 30.96 0.512370 19.15 17.02 0.88 1007.68 0.70 752.70 0.80 0.00 0.00 0.00 0.60 0.51 0.00 0.52 5.77 0.60 0.30 70.14 0.706534 31.11 0.512369 19.22 17.03 0.88 1006.96 0.71 755.02 0.79 0.00 0.00 0.00 0.60 0.52 0.00 0.52 5.77 0.60 0.30 68.63 0.706542 31.25 0.512368 19.29 17.03 0.88 1006.23 0.71 757.42 0.79 0.00 0.00 0.00 0.60 0.52 0.01 0.53 5.77 0.60 0.30 67.14 0.706551 31.40 0.512367 19.36 17.03 0.88 1005.50 0.71 759.93 0.78 0.00 0.00 0.00 0.59 0.53 0.01 0.54 5.77 0.59 0.30 65.66 0.706562 31.56 0.512366 19.44 17.03 0.88 1004.77 0.71 762.59 0.78 0.00 0.01 0.01 0.59 0.54 0.01 0.54 5.76 0.59 0.31 64.20 0.706574 31.72 0.512364 19.51 17.04 0.88 1004.04 0.71 765.44 0.78 0.00 0.01 0.01 0.58 0.54 0.01 0.55 5.76 0.58 0.31 62.76 0.706589 31.88 0.512362 19.58 17.04 0.88 1003.31 0.71 768.52 0.77 0.00 0.01 0.01 0.58 0.55 0.01 0.56 5.76 0.58 0.31 61.34 0.706607 32.05 0.512360 19.66 17.04 0.88 1002.58 0.72 771.88 0.77 0.00 0.01 0.01 0.57 0.55 0.01 0.57 5.75 0.57 0.32 59.93 0.706628 32.22 0.512358 19.74 17.05 0.88 1001.86 0.72 775.56 0.77 0.01 0.01 0.01 0.57 0.56 0.02 0.58 5.75 0.57 0.33 58.54 0.706655 32.40 0.512355 19.82 17.05 0.87 1001.13 0.72 779.58 0.77 0.01 0.01 0.01 0.56 0.56 0.02 0.59 5.74 0.56 0.33 57.18 0.706689 32.59 0.512351 19.90 17.06 0.87 1000.40 0.73 783.91 0.77 0.01 0.01 0.01 0.56 0.57 0.02 0.60 5.73 0.56 0.34 55.84 0.706730 32.79 0.512347 19.98 17.07 0.87 999.67 0.73 788.54 0.77 0.01 0.01 0.01 0.55 0.58 0.03 0.61 5.72 0.55 0.35 54.52 0.706782 33.01 0.512342 20.06 17.07 0.87 998.94 0.73 793.38 0.77 0.01 0.01 0.01 0.55 0.58 0.04 0.62 5.71 0.55 0.37 53.23 0.706844 33.23 0.512336 20.15 17.08 0.87 998.21 0.74 798.36 0.77 0.01 0.02 0.02 0.55 0.59 0.04 0.63 5.70 0.55 0.38 51.97 0.706919 33.47 0.512329 20.23 17.10 0.87 997.48 0.74 803.36 0.78 0.01 0.02 0.02 0.54 0.60 0.05 0.64 5.68 0.54 0.39 50.75 0.707008 33.71 0.512321 20.32 17.11 0.87 996.75 0.74 808.28 0.78 0.01 0.02 0.02 0.54 0.60 0.05 0.66 5.67 0.54 0.40 49.56 0.707110 33.98 0.512312 20.41 17.13 0.87 996.03 0.75 813.04 0.78 0.02 0.02 0.02 0.53 0.61 0.06 0.67 5.65 0.53 0.42 48.41 0.707225 34.25 0.512302 20.50 17.14 0.87 995.30 0.75 817.56 0.79 0.02 0.03 0.03 0.53 0.62 0.06 0.68 5.63 0.53 0.43 47.29 0.707352 34.53 0.512292 20.59 17.16 0.87 994.57 0.75 821.82 0.79 0.02 0.03 0.03 0.52 0.62 0.07 0.69 5.60 0.52 0.44 46.20 0.707489 34.82 0.512281 20.68 17.18 0.87 993.84 0.75 825.78 0.79 0.02 0.03 0.03 0.52 0.63 0.07 0.70 5.58 0.52 0.45 45.15 0.707634 35.11 0.512270 20.77 17.20 0.87 993.11 0.76 829.44 0.79 0.02 0.04 0.04 0.51 0.64 0.08 0.71 5.56 0.51 0.46 44.13 0.707787 35.41 0.512259 20.86 17.22 0.87 992.38 0.76 832.83 0.79 0.03 0.04 0.04 0.51 0.64 0.08 0.72 5.53 0.51 0.46 43.15 0.707945 35.71 0.512248 20.95 17.24 0.87 991.65 0.76 835.95 0.79 0.03 0.04 0.04 0.50 0.65 0.08 0.73 5.51 0.50 0.47 42.19 0.708108 36.01 0.512237 21.04 17.27 0.87 990.93 0.76 838.84 0.79 0.03 0.05 0.05 0.50 0.66 0.09 0.74 5.49 0.50 0.48 41.25 0.708275 36.31 0.512225 21.13 17.29 0.87 990.20 0.76 841.52 0.79 0.03 0.05 0.05 0.49 0.66 0.09 0.75 5.46 0.49 0.48 40.35 0.708446 36.62 0.512215 21.22 17.31 0.87 989.47 0.77 844.02 0.79 0.04 0.06 0.06 0.49 0.67 0.09 0.76 5.44 0.49 0.48 39.47 0.708620 36.92 0.512204 21.31 17.33 0.87 988.74 0.77 846.37 0.79 0.04 0.06 0.06 0.49 0.68 0.09 0.77 5.41 0.49 0.49 38.61 0.708798 37.23 0.512193 21.40 17.35 0.87 988.01 0.77 848.58 0.79 0.04 0.06 0.06 0.48 0.68 0.09 0.77 5.39 0.48 0.49 37.78 0.708980 37.54 0.512183 21.49 17.37 0.87 987.28 0.77 850.68 0.78 0.04 0.07 0.07 0.48 0.69 0.09 0.78 5.36 0.48 0.49 36.98 0.709166 37.85 0.512172 21.59 17.39 0.86 986.55 0.77 852.68 0.78 0.05 0.07 0.07 0.47 0.70 0.09 0.79 5.34 0.47 0.49 36.20 0.709358 38.16 0.512162 21.68 17.41 0.86 985.83 0.77 854.59 0.78 0.05 0.07 0.07 0.47 0.70 0.09 0.80 5.32 0.47 0.49 35.45 0.709554 38.47 0.512151 21.77 17.43 0.86 985.10 0.78 856.43 0.78 0.05 0.08 0.08 0.46 0.71 0.09 0.81 5.29 0.46 0.49 34.72 0.709756 38.78 0.512141 21.86 17.45 0.86 984.37 0.78 858.21 0.77 0.05 0.08 0.08 0.46 0.72 0.09 0.81 5.27 0.46 0.50 34.01 0.709964 39.10 0.512130 21.95 17.47 0.86 983.64 0.78 859.93 0.77 0.06 0.09 0.09 0.45 0.72 0.10 0.82 5.24 0.45 0.50 33.33 0.710177 39.42 0.512120 22.05 17.49 0.86 982.91 0.78 861.60 0.77 0.06 0.09 0.09 0.45 0.73 0.10 0.83 5.21 0.45 0.50 32.68 0.710398 39.74 0.512110 22.14 17.52 0.86 982.18 0.78 863.23 0.77 0.06 0.09 0.09 0.44 0.74 0.10 0.83 5.19 0.44 0.50 32.05 0.710625 40.06 0.512099 22.23 17.54 0.86 981.45 0.78 864.82 0.76 0.07 0.10 0.10 0.44 0.75 0.10 0.84 5.16 0.44 0.50 31.44 0.710859 40.39 0.512089 22.32 17.56 0.86 980.73 0.78 866.38 0.76 0.07 0.10 0.10 0.44 0.75 0.10 0.85 5.13 0.44 0.50 30.86 0.711100 40.71 0.512078 22.41 17.58 0.86 980.00 0.78 867.90 0.76 0.07 0.11 0.11 0.43 0.76 0.10 0.85 5.11 0.43 0.50 30.30 0.711347 41.04 0.512068 22.50 17.60 0.86 979.27 0.78 869.39 0.76 0.07 0.11 0.11 0.43 0.77 0.10 0.86 5.08 0.43 0.50 29.77 0.711601 41.37 0.512057 22.59 17.63

142 0.86 978.54 0.79 870.85 0.75 0.08 0.12 0.12 0.42 0.77 0.10 0.87 5.05 0.42 0.50 29.26 0.711862 41.70 0.512047 22.68 17.65 0.86 977.81 0.79 872.29 0.75 0.08 0.12 0.12 0.42 0.78 0.10 0.88 5.02 0.42 0.50 28.77 0.712130 42.04 0.512036 22.77 17.67 0.86 977.08 0.79 873.70 0.75 0.08 0.12 0.12 0.41 0.79 0.10 0.88 4.99 0.41 0.50 28.30 0.712403 42.37 0.512025 22.86 17.70 0.86 976.35 0.79 875.08 0.75 0.09 0.13 0.13 0.41 0.79 0.10 0.89 4.96 0.41 0.50 27.86 0.712683 42.71 0.512015 22.95 17.72 0.86 975.63 0.79 876.45 0.75 0.09 0.13 0.13 0.40 0.80 0.10 0.90 4.93 0.40 0.50 27.44 0.712968 43.04 0.512004 23.04 17.74 0.86 974.90 0.79 877.79 0.74 0.09 0.14 0.14 0.40 0.81 0.10 0.90 4.90 0.40 0.50 27.05 0.713258 43.38 0.511994 23.13 17.77 0.86 974.17 0.79 879.11 0.74 0.10 0.14 0.14 0.39 0.81 0.10 0.91 4.87 0.39 0.50 26.67 0.713553 43.71 0.511983 23.21 17.79 0.86 973.44 0.79 880.41 0.74 0.10 0.15 0.15 0.39 0.82 0.10 0.92 4.84 0.39 0.50 26.32 0.713853 44.05 0.511972 23.30 17.82 0.86 972.71 0.79 881.69 0.74 0.10 0.15 0.15 0.39 0.83 0.10 0.92 4.81 0.39 0.50 25.98 0.714156 44.39 0.511962 23.38 17.84 0.85 971.98 0.79 882.95 0.74 0.11 0.16 0.16 0.38 0.83 0.10 0.93 4.78 0.38 0.50 25.67 0.714463 44.72 0.511951 23.46 17.86 0.85 971.25 0.79 884.20 0.74 0.11 0.16 0.16 0.38 0.84 0.10 0.94 4.74 0.38 0.50 25.38 0.714772 45.06 0.511941 23.55 17.89 0.85 970.53 0.80 885.42 0.74 0.11 0.17 0.17 0.37 0.85 0.10 0.94 4.71 0.37 0.50 25.10 0.715084 45.39 0.511930 23.63 17.91 0.85 969.80 0.80 886.63 0.73 0.12 0.17 0.17 0.37 0.85 0.10 0.95 4.68 0.37 0.50 24.85 0.715398 45.73 0.511920 23.71 17.94 0.85 969.07 0.80 887.82 0.73 0.12 0.18 0.18 0.36 0.86 0.10 0.95 4.65 0.36 0.50 24.61 0.715713 46.06 0.511909 23.79 17.96 0.85 968.34 0.80 889.00 0.73 0.12 0.19 0.19 0.36 0.86 0.10 0.96 4.61 0.36 0.50 24.39 0.716028 46.39 0.511899 23.86 17.99 0.85 967.61 0.80 890.16 0.73 0.13 0.19 0.19 0.36 0.87 0.10 0.97 4.58 0.36 0.50 24.18 0.716343 46.72 0.511889 23.94 18.01 0.85 966.88 0.80 891.30 0.73 0.13 0.20 0.20 0.35 0.88 0.10 0.97 4.55 0.35 0.50 24.00 0.716658 47.04 0.511879 24.01 18.04 0.85 966.15 0.80 892.43 0.73 0.13 0.20 0.20 0.35 0.88 0.10 0.98 4.52 0.35 0.50 23.83 0.716972 47.37 0.511869 24.09 18.06 0.85 965.43 0.80 893.55 0.73 0.14 0.21 0.21 0.34 0.89 0.10 0.99 4.48 0.34 0.50 23.68 0.717285 47.69 0.511858 24.16 18.09 0.85 964.70 0.80 894.64 0.73 0.14 0.21 0.21 0.34 0.90 0.10 0.99 4.45 0.34 0.50 23.54 0.717595 48.01 0.511849 24.23 18.11 0.85 963.97 0.80 895.73 0.73 0.15 0.22 0.22 0.33 0.90 0.10 1.00 4.42 0.33 0.50 23.41 0.717903 48.33 0.511839 24.30 18.14 0.85 963.24 0.80 896.80 0.73 0.15 0.23 0.23 0.33 0.91 0.10 1.00 4.38 0.33 0.50 23.31 0.718208 48.64 0.511829 24.37 18.16 0.85 962.51 0.80 897.86 0.73 0.15 0.23 0.23 0.33 0.91 0.10 1.01 4.35 0.33 0.50 23.21 0.718509 48.95 0.511819 24.43 18.19 0.85 961.78 0.80 898.91 0.73 0.16 0.24 0.24 0.32 0.92 0.10 1.02 4.31 0.32 0.50 23.13 0.718807 49.26 0.511810 24.50 18.21 0.85 961.05 0.81 899.94 0.73 0.16 0.24 0.24 0.32 0.93 0.10 1.02 4.28 0.32 0.50 23.06 0.719100 49.56 0.511800 24.56 18.24 0.85 960.33 0.81 900.96 0.73 0.17 0.25 0.25 0.31 0.93 0.10 1.03 4.25 0.31 0.50 23.01 0.719389 49.86 0.511791 24.62 18.26 0.85 959.60 0.81 901.97 0.73 0.17 0.26 0.26 0.31 0.94 0.10 1.03 4.21 0.31 0.50 22.97 0.719673 50.15 0.511781 24.68 18.29 0.85 958.87 0.81 902.97 0.73 0.17 0.26 0.26 0.31 0.94 0.10 1.04 4.18 0.31 0.50 22.94 0.719952 50.44 0.511772 24.74 18.31 0.85 958.14 0.81 903.95 0.73 0.18 0.27 0.27 0.30 0.95 0.10 1.05 4.15 0.30 0.50 22.92 0.720226 50.73 0.511763 24.80 18.33 0.84 957.41 0.81 904.93 0.73 0.18 0.27 0.27 0.30 0.96 0.10 1.05 4.11 0.30 0.50 22.91 0.720493 51.01 0.511754 24.85 18.36 0.84 956.68 0.81 905.89 0.73 0.19 0.28 0.28 0.30 0.96 0.10 1.06 4.08 0.30 0.50 22.92 0.720755 51.29 0.511745 24.90 18.38 0.84 955.95 0.81 906.85 0.73 0.19 0.29 0.29 0.29 0.97 0.10 1.06 4.05 0.29 0.50 22.93 0.721012 51.57 0.511737 24.95 18.41 0.84 955.23 0.81 907.79 0.73 0.20 0.29 0.29 0.29 0.97 0.10 1.07 4.02 0.29 0.50 22.95 0.721261 51.84 0.511728 25.00 18.43 0.84 954.50 0.81 908.73 0.73 0.20 0.30 0.30 0.28 0.98 0.10 1.08 3.98 0.28 0.50 22.99 0.721505 52.10 0.511719 25.05 18.45 0.84 953.77 0.81 909.65 0.73 0.20 0.31 0.31 0.28 0.98 0.10 1.08 3.95 0.28 0.50 23.03 0.721743 52.36 0.511711 25.10 18.48 0.84 953.04 0.81 910.57 0.73 0.21 0.31 0.31 0.28 0.99 0.10 1.09 3.92 0.28 0.50 23.09 0.721974 52.61 0.511703 25.14 18.50 0.84 952.31 0.81 911.47 0.74 0.21 0.32 0.32 0.27 1.00 0.10 1.09 3.89 0.27 0.50 23.15 0.722198 52.86 0.511695 25.18 18.52 0.84 951.58 0.81 912.37 0.74 0.22 0.33 0.33 0.27 1.00 0.10 1.10 3.85 0.27 0.50 23.22 0.722417 53.11 0.511687 25.23 18.55 0.84 950.85 0.81 913.26 0.74 0.22 0.33 0.33 0.27 1.01 0.10 1.10 3.82 0.27 0.50 23.30 0.722629 53.35 0.511679 25.26 18.57 0.84 950.13 0.81 914.14 0.74 0.23 0.34 0.34 0.26 1.01 0.10 1.11 3.79 0.26 0.50 23.39 0.722834 53.58 0.511671 25.30 18.59 0.84 949.40 0.82 915.01 0.74 0.23 0.35 0.35 0.26 1.02 0.10 1.11 3.76 0.26 0.50 23.49 0.723034 53.81 0.511663 25.34 18.62 0.84 948.67 0.82 915.87 0.74 0.24 0.35 0.35 0.25 1.02 0.10 1.12 3.73 0.25 0.50 23.60 0.723227 54.03 0.511655 25.37 18.64 0.84 947.94 0.82 916.73 0.74 0.24 0.36 0.36 0.25 1.03 0.10 1.12 3.70 0.25 0.50 23.71 0.723414 54.25 0.511648 25.40 18.66 0.84 947.21 0.82 917.58 0.74 0.24 0.37 0.37 0.25 1.03 0.10 1.13 3.66 0.25 0.50 23.83 0.723595 54.46 0.511640 25.43 18.68 0.84 946.48 0.82 918.42 0.75 0.25 0.37 0.37 0.24 1.04 0.10 1.13 3.63 0.24 0.50 23.96 0.723770 54.66 0.511633 25.46 18.70 0.84 945.75 0.82 919.26 0.75 0.25 0.38 0.38 0.24 1.04 0.10 1.14 3.60 0.24 0.50 24.09 0.723939 54.86 0.511626 25.49 18.73 0.84 945.03 0.82 920.09 0.75 0.26 0.39 0.39 0.24 1.05 0.10 1.14 3.57 0.24 0.50 24.23 0.724102 55.06 0.511619 25.51 18.75 0.84 944.30 0.82 920.91 0.75 0.26 0.39 0.39 0.23 1.05 0.10 1.15 3.54 0.23 0.50 24.38 0.724260 55.25 0.511612 25.54 18.77 0.84 943.57 0.82 921.72 0.75 0.27 0.40 0.40 0.23 1.06 0.10 1.15 3.51 0.23 0.50 24.54 0.724413 55.43 0.511605 25.56 18.79 0.83 942.84 0.82 922.53 0.76 0.27 0.41 0.41 0.23 1.06 0.10 1.16 3.49 0.23 0.50 24.70 0.724560 55.61 0.511598 25.58 18.81 0.83 942.11 0.82 923.33 0.76 0.28 0.41 0.41 0.22 1.07 0.10 1.16 3.46 0.22 0.50 24.87 0.724701 55.78 0.511592 25.60 18.83 0.83 941.38 0.82 924.13 0.76 0.28 0.42 0.42 0.22 1.07 0.10 1.17 3.43 0.22 0.50 25.04 0.724838 55.95 0.511585 25.62 18.85 0.83 940.65 0.82 924.92 0.76 0.29 0.43 0.43 0.22 1.08 0.10 1.17 3.40 0.22 0.50 25.22 0.724970 56.11 0.511578 25.63 18.87 0.83 939.93 0.82 925.71 0.76 0.29 0.44 0.44 0.21 1.08 0.10 1.18 3.37 0.21 0.50 25.41 0.725097 56.26 0.511572 25.64 18.89 0.83 939.20 0.82 926.49 0.77 0.30 0.44 0.44 0.21 1.09 0.10 1.18 3.34 0.21 0.50 25.60 0.725219 56.41 0.511566 25.66 18.91 0.83 938.47 0.82 927.27 0.77 0.30 0.45 0.45 0.21 1.09 0.10 1.19 3.32 0.21 0.50 25.80 0.725337 56.56 0.511560 25.67 18.93 0.83 937.74 0.82 928.04 0.77 0.30 0.46 0.46 0.21 1.10 0.10 1.19 3.29 0.21 0.50 26.00 0.725451 56.69 0.511554 25.67 18.95 0.83 937.01 0.82 928.80 0.77 0.31 0.46 0.46 0.20 1.10 0.10 1.20 3.26 0.20 0.50 26.21 0.725560 56.83 0.511548 25.68 18.97 0.83 936.28 0.83 929.56 0.78 0.31 0.47 0.47 0.20 1.10 0.10 1.20 3.23 0.20 0.50 26.42 0.725665 56.95 0.511542 25.69 18.99 0.83 935.55 0.83 930.32 0.78 0.32 0.48 0.48 0.20 1.11 0.10 1.21 3.21 0.20 0.50 26.64 0.725767 57.07 0.511536 25.69 19.01 0.83 934.83 0.83 931.07 0.78 0.32 0.48 0.48 0.19 1.11 0.10 1.21 3.18 0.19 0.50 26.87 0.725864 57.19 0.511530 25.69 19.03 0.83 934.10 0.83 931.82 0.79 0.33 0.49 0.49 0.19 1.12 0.10 1.21 3.16 0.19 0.50 27.10 0.725958 57.30 0.511525 25.70 19.04 0.83 933.37 0.83 932.57 0.79 0.33 0.50 0.50 0.19 1.12 0.10 1.22 3.13 0.19 0.50 27.33 0.726049 57.41 0.511519 25.70 19.06

143 EC-RAXFC Results - Melts Page MODEL C - Swan Lake Flat

Equilibration Parameters tlm 1184 degC 18O/16O in magma 5.8 Magma a 450 Mro 0.5 Element Name Sr Nd Pb Teq Norm 0.816 tmo 1184 degC 18O/16O in assimilant 0.5 Magma b -11 Episodic Recharge Magma: conc. 419 17 2 Teq deg C 915.88256 tla 1129 degC 18O/16O in recharge 5.8 Assimilant a 400 Episode deltaMri Tm,i mr,i d,i bulk Dmo 4 0.6 0.5 Mm 0.608820503 tao 450 degC Oxygen conc magma 0.47 Assimilant b -11 1 0.2 1000 0.3 2 enthalpy 0 0 0 Mao 1.759219249 tlr 1184 degC Oxygen conc assimilant 0.5 Recharge Magma a 450 2 0.2 1175 0.3 2 Assimilant: conc. 255 44.5 8.3 Ma* 0.414479854 tro 1184 degC Oxygen conc recharge 0.47 Recharge Magma b -11 3 0.1 1155 0.3 2 bulk Dao 6 0.7 0.7 Mc 1.2090232 ts 750 degC enthalpy 0 0 0 Men 0.096636151 cpm 1100 J/kg K Recharge: conc. 419 17 2 Ms 1.305659351 cpa 1000 J/kg K bulk Dro 4 0.5 0.5 fa 0.235604433 cpr 1100 J/kg K enthalpy 0 0 0 fm 0.129560433 hm 400000 J/kg Isotope Name 87Sr/86Sr 143Nd/144Nd 206Pb/204Pb fr 0.129560433 ha 350000 J/kg ratio in magma 0.7054 0.512483 16.79 hr 400000 J/kg ratio in assimilant 0.728666 0.51112 17.62 X 1 Normalized fraction of Wallrock melt ratio in recharge 0.7054 0.512483 16.79 mixed into Magma body

Norm T T magma Norm T T assim magma (deg C) assim (deg C) Mm fa Ma* X Ma* fm Mc Men Ms delO18 fr Mr Sr 87Sr/86Sr Nd 143Nd/144Nd Pb 206Pb/204Pb

1.00 1184.00 0.50 450.00 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 419.00 0.7054000 17.00 0.5124830 2.00 16.79 1.00 1183.27 0.50 450.49 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.82 0.7054000 17.00 0.5124830 2.00 16.79 1.00 1182.54 0.50 450.98 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.64 0.7054000 17.00 0.5124830 2.00 16.79 1.00 1181.81 0.50 451.47 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.45 0.7054000 17.00 0.5124830 2.00 16.79 1.00 1181.09 0.50 451.96 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.26 0.7054000 17.00 0.5124830 2.00 16.79 1.00 1180.36 0.50 452.46 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.06 0.7054000 17.01 0.5124830 2.00 16.79 1.00 1179.63 0.50 452.96 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 417.85 0.7054000 17.01 0.5124830 2.00 16.79 1.00 1178.90 0.50 453.47 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 417.62 0.7054000 17.01 0.5124830 2.00 16.79 1.00 1178.17 0.50 453.99 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 417.39 0.7054000 17.01 0.5124830 2.00 16.79 1.00 1177.44 0.50 454.53 1.02 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.02 417.14 0.7054000 17.01 0.5124830 2.00 16.79 1.00 1176.71 0.50 455.08 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.03 416.87 0.7054000 17.01 0.5124830 2.00 16.79 0.99 1175.99 0.50 455.64 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.04 416.59 0.7054000 17.01 0.5124830 2.00 16.79 0.99 1175.26 0.50 456.23 1.04 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.05 416.30 0.7054000 17.02 0.5124830 2.00 16.79 0.99 1174.53 0.50 456.83 1.05 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.06 415.99 0.7054000 17.02 0.5124830 2.00 16.79 0.99 1173.80 0.50 457.46 1.07 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.07 415.68 0.7054000 17.02 0.5124830 2.00 16.79 0.99 1173.07 0.50 458.11 1.08 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.08 415.35 0.7054000 17.02 0.5124830 2.00 16.79 0.99 1172.34 0.50 458.77 1.09 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.09 415.02 0.7054000 17.02 0.5124830 2.00 16.79 0.99 1171.61 0.50 459.44 1.10 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.11 414.70 0.7054000 17.03 0.5124830 2.00 16.79 0.99 1170.89 0.50 460.12 1.12 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.12 414.37 0.7054000 17.03 0.5124830 2.00 16.79 0.99 1170.16 0.50 460.80 1.13 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.13 414.05 0.7054000 17.03 0.5124830 2.00 16.79 0.99 1169.43 0.50 461.49 1.14 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.14 413.73 0.7054000 17.03 0.5124830 2.00 16.79 0.99 1168.70 0.50 462.17 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.15 413.42 0.7054000 17.03 0.5124830 2.00 16.79 0.99 1167.97 0.51 462.85 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.16 413.12 0.7054000 17.03 0.5124830 2.00 16.79 0.99 1167.24 0.51 463.52 1.16 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 412.81 0.7054000 17.04 0.5124830 2.00 16.79 0.99 1166.51 0.51 464.19 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 412.51 0.7054000 17.04 0.5124830 2.01 16.79 0.99 1165.79 0.51 464.85 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 412.21 0.7054000 17.04 0.5124830 2.01 16.79 0.99 1165.06 0.51 465.51 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 411.91 0.7054000 17.04 0.5124830 2.01 16.79 0.99 1164.33 0.51 466.16 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 411.62 0.7054000 17.04 0.5124830 2.01 16.79 0.99 1163.60 0.51 466.81 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.19 411.32 0.7054000 17.04 0.5124830 2.01 16.79 0.99 1162.87 0.51 467.45 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 411.02 0.7054000 17.05 0.5124830 2.01 16.79 0.99 1162.14 0.51 468.10 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 410.71 0.7054000 17.05 0.5124830 2.01 16.79 0.98 1161.41 0.51 468.74 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 410.40 0.7054000 17.05 0.5124830 2.01 16.79 0.98 1160.69 0.51 469.38 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 410.09 0.7054000 17.05 0.5124830 2.01 16.79 0.98 1159.96 0.51 470.03 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 409.77 0.7054000 17.05 0.5124830 2.01 16.79 0.98 1159.23 0.51 470.69 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 409.45 0.7054000 17.06 0.5124830 2.01 16.79 0.98 1158.50 0.51 471.35 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 409.12 0.7054000 17.06 0.5124830 2.01 16.79 0.98 1157.77 0.51 472.03 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 408.78 0.7054000 17.06 0.5124830 2.01 16.79 0.98 1157.04 0.51 472.73 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 408.43 0.7054000 17.06 0.5124830 2.01 16.79 0.98 1156.31 0.51 473.44 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 408.07 0.7054000 17.06 0.5124830 2.01 16.79 0.98 1155.59 0.51 474.17 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 407.70 0.7054000 17.07 0.5124830 2.01 16.79 0.98 1154.86 0.51 474.93 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 407.32 0.7054000 17.07 0.5124830 2.01 16.79 0.98 1154.13 0.51 475.70 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.23 406.93 0.7054000 17.07 0.5124830 2.01 16.79 0.98 1153.40 0.51 476.48 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 406.54 0.7054000 17.07 0.5124830 2.01 16.79 0.98 1152.67 0.52 477.28 1.23 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 406.14 0.7054000 17.07 0.5124830 2.01 16.79 0.98 1151.94 0.52 478.09 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.25 405.73 0.7054000 17.08 0.5124830 2.01 16.79 0.98 1151.21 0.52 478.90 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 405.32 0.7054000 17.08 0.5124830 2.01 16.79 0.98 1150.49 0.52 479.71 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 404.90 0.7054000 17.08 0.5124830 2.01 16.79 0.98 1149.76 0.52 480.51 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 404.48 0.7054000 17.08 0.5124830 2.01 16.79 0.98 1149.03 0.52 481.31 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 404.06 0.7054000 17.09 0.5124830 2.01 16.79 0.98 1148.30 0.52 482.10 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 403.64 0.7054000 17.09 0.5124830 2.01 16.79 0.98 1147.57 0.52 482.88 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 403.21 0.7054000 17.09 0.5124830 2.01 16.79 0.97 1146.84 0.52 483.65 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 402.77 0.7054000 17.09 0.5124830 2.01 16.79 0.97 1146.11 0.52 484.41 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.29 402.33 0.7054000 17.10 0.5124830 2.01 16.79 0.97 1145.39 0.52 485.17 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 401.89 0.7054000 17.10 0.5124830 2.01 16.79 0.97 1144.66 0.52 485.91 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 401.44 0.7054000 17.10 0.5124830 2.01 16.79 0.97 1143.93 0.52 486.66 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 400.99 0.7054000 17.10 0.5124830 2.01 16.79 0.97 1143.20 0.52 487.39 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 400.53 0.7054000 17.11 0.5124830 2.02 16.79 0.97 1142.47 0.52 488.13 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 400.06 0.7054000 17.11 0.5124830 2.02 16.79 0.97 1141.74 0.52 488.86 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 399.59 0.7054000 17.11 0.5124830 2.02 16.79 0.97 1141.01 0.52 489.58 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 399.11 0.7054000 17.12 0.5124830 2.02 16.79 0.97 1140.29 0.52 490.31 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 398.62 0.7054000 17.12 0.5124830 2.02 16.79 0.97 1139.56 0.52 491.04 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 398.13 0.7054000 17.12 0.5124830 2.02 16.79 0.97 1138.83 0.52 491.76 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 397.62 0.7054000 17.12 0.5124830 2.02 16.79 0.97 1138.10 0.53 492.49 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 397.11 0.7054000 17.13 0.5124830 2.02 16.79 0.97 1137.37 0.53 493.21 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 396.59 0.7054000 17.13 0.5124830 2.02 16.79 0.97 1136.64 0.53 493.94 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 396.07 0.7054000 17.13 0.5124830 2.02 16.79 0.97 1135.91 0.53 494.67 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 395.53 0.7054000 17.14 0.5124830 2.02 16.79 0.97 1135.19 0.53 495.40 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 394.98 0.7054000 17.14 0.5124830 2.02 16.79 0.97 1134.46 0.53 496.13 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 394.43 0.7054000 17.14 0.5124830 2.02 16.79 0.97 1133.73 0.53 496.86 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 393.87 0.7054000 17.15 0.5124830 2.02 16.79 0.97 1133.00 0.53 497.59 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 393.29 0.7054000 17.15 0.5124830 2.02 16.79 0.96 1132.27 0.53 498.33 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 392.71 0.7054000 17.15 0.5124830 2.02 16.79 0.96 1131.54 0.53 499.07 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 392.12 0.7054000 17.16 0.5124830 2.02 16.79 0.96 1130.81 0.53 499.81 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 391.52 0.7054000 17.16 0.5124830 2.02 16.79 0.96 1130.09 0.53 500.55 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 390.91 0.7054000 17.16 0.5124830 2.02 16.79 0.96 1129.36 0.53 501.30 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 390.29 0.7054000 17.17 0.5124830 2.02 16.79 0.96 1128.63 0.53 502.05 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 389.65 0.7054000 17.17 0.5124830 2.02 16.79 0.96 1127.90 0.53 502.80 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 389.01 0.7054000 17.17 0.5124830 2.02 16.79 0.96 1127.17 0.53 503.55 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 388.36 0.7054000 17.18 0.5124830 2.03 16.79 0.96 1126.44 0.53 504.31 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 387.70 0.7054000 17.18 0.5124830 2.03 16.79 0.96 1125.71 0.53 505.07 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 387.02 0.7054000 17.19 0.5124830 2.03 16.79 0.96 1124.99 0.53 505.83 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 386.34 0.7054000 17.19 0.5124830 2.03 16.79 0.96 1124.26 0.54 506.59 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 385.64 0.7054000 17.19 0.5124830 2.03 16.79 0.96 1123.53 0.54 507.36 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 384.93 0.7054000 17.20 0.5124830 2.03 16.79 0.96 1122.80 0.54 508.13 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 384.21 0.7054000 17.20 0.5124830 2.03 16.79 0.96 1122.07 0.54 508.90 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.05 5.80 0.97 0.30 383.48 0.7054000 17.21 0.5124830 2.03 16.79 0.96 1121.34 0.54 509.68 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 382.74 0.7054000 17.21 0.5124830 2.03 16.79 0.96 1120.61 0.54 510.46 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 381.99 0.7054000 17.22 0.5124830 2.03 16.79

144 0.96 1119.88 0.54 511.24 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 381.22 0.7054000 17.22 0.5124830 2.03 16.79 0.96 1119.16 0.54 512.03 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 380.45 0.7054000 17.23 0.5124830 2.03 16.79 0.96 1118.43 0.54 512.82 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 379.65 0.7054000 17.23 0.5124830 2.03 16.79 0.95 1117.70 0.54 513.62 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 378.85 0.7054000 17.24 0.5124830 2.03 16.79 0.95 1116.97 0.54 514.41 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 378.04 0.7054000 17.24 0.5124830 2.03 16.79 0.95 1116.24 0.54 515.21 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 377.21 0.7054000 17.25 0.5124830 2.04 16.79 0.95 1115.51 0.54 516.02 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 376.37 0.7054000 17.25 0.5124830 2.04 16.79 0.95 1114.78 0.54 516.82 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 375.51 0.7054000 17.26 0.5124830 2.04 16.79 0.95 1114.06 0.54 517.64 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 374.65 0.7054000 17.26 0.5124830 2.04 16.79 0.95 1113.33 0.54 518.45 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 373.76 0.7054000 17.27 0.5124830 2.04 16.79 0.95 1112.60 0.54 519.27 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 372.87 0.7054000 17.27 0.5124830 2.04 16.79 0.95 1111.87 0.54 520.09 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 371.96 0.7054000 17.28 0.5124830 2.04 16.79 0.95 1111.14 0.54 520.92 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 371.04 0.7054000 17.28 0.5124830 2.04 16.79 0.95 1110.41 0.55 521.75 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 370.10 0.7054000 17.29 0.5124830 2.04 16.79 0.95 1109.68 0.55 522.58 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 369.15 0.7054000 17.29 0.5124830 2.04 16.79 0.95 1108.96 0.55 523.42 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 368.19 0.7054000 17.30 0.5124830 2.04 16.79 0.95 1108.23 0.55 524.26 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 367.21 0.7054000 17.31 0.5124830 2.04 16.79 0.95 1107.50 0.55 525.11 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 366.22 0.7054000 17.31 0.5124830 2.05 16.79 0.95 1106.77 0.55 525.96 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 365.21 0.7054000 17.32 0.5124830 2.05 16.79 0.95 1106.04 0.55 526.82 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 364.18 0.7054000 17.33 0.5124830 2.05 16.79 0.95 1105.31 0.55 527.68 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 363.14 0.7054000 17.33 0.5124830 2.05 16.79 0.95 1104.58 0.55 528.54 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 362.09 0.7054000 17.34 0.5124830 2.05 16.79 0.95 1103.86 0.55 529.41 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 361.02 0.7054000 17.35 0.5124830 2.05 16.79 0.94 1103.13 0.55 530.29 1.24 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 359.94 0.7054000 17.35 0.5124830 2.05 16.79 0.94 1102.40 0.55 531.16 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 358.83 0.7054000 17.36 0.5124830 2.05 16.79 0.94 1101.67 0.55 532.05 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 357.72 0.7054000 17.37 0.5124830 2.05 16.79 0.94 1100.94 0.55 532.94 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 356.59 0.7054000 17.37 0.5124830 2.05 16.79 0.94 1100.21 0.55 533.83 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 355.44 0.7054000 17.38 0.5124830 2.06 16.79 0.94 1099.48 0.55 534.73 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 354.27 0.7054000 17.39 0.5124830 2.06 16.79 0.94 1098.76 0.56 535.63 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 353.09 0.7054000 17.40 0.5124830 2.06 16.79 0.94 1098.03 0.56 536.54 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 351.89 0.7054000 17.41 0.5124830 2.06 16.79 0.94 1097.30 0.56 537.45 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 350.68 0.7054000 17.41 0.5124830 2.06 16.79 0.94 1096.57 0.56 538.37 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 349.44 0.7054000 17.42 0.5124830 2.06 16.79 0.94 1095.84 0.56 539.29 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 348.19 0.7054000 17.43 0.5124830 2.06 16.79 0.94 1095.11 0.56 540.22 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 346.93 0.7054000 17.44 0.5124830 2.06 16.79 0.94 1094.38 0.56 541.15 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 345.64 0.7054000 17.45 0.5124830 2.07 16.79 0.94 1093.66 0.56 542.09 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 344.34 0.7054000 17.46 0.5124830 2.07 16.79 0.94 1092.93 0.56 543.04 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 343.03 0.7054000 17.47 0.5124830 2.07 16.79 0.94 1092.20 0.56 543.99 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 341.69 0.7054000 17.47 0.5124830 2.07 16.79 0.94 1091.47 0.56 544.95 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 340.34 0.7054000 17.48 0.5124830 2.07 16.79 0.94 1090.74 0.56 545.91 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.10 5.80 0.93 0.30 338.96 0.7054000 17.49 0.5124830 2.07 16.79 0.94 1090.01 0.56 546.88 1.21 0.00 0.00 0.00 0.92 0.09 0.00 0.10 5.80 0.92 0.30 337.57 0.7054000 17.50 0.5124830 2.07 16.79 0.94 1089.28 0.56 547.85 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 336.17 0.7054000 17.51 0.5124830 2.07 16.79 0.93 1088.56 0.56 548.83 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 334.74 0.7054000 17.52 0.5124830 2.08 16.79 0.93 1087.83 0.56 549.82 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 333.30 0.7054000 17.53 0.5124829 2.08 16.79 0.93 1087.10 0.57 550.81 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 331.83 0.7054000 17.54 0.5124829 2.08 16.79 0.93 1086.37 0.57 551.81 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 330.35 0.7054000 17.55 0.5124829 2.08 16.79 0.93 1085.64 0.57 552.81 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 328.85 0.7054000 17.56 0.5124829 2.08 16.79 0.93 1084.91 0.57 553.83 1.20 0.00 0.00 0.00 0.92 0.11 0.00 0.11 5.80 0.92 0.30 327.33 0.7054000 17.57 0.5124829 2.08 16.79 0.93 1084.18 0.57 554.84 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 325.80 0.7054000 17.59 0.5124829 2.09 16.79 0.93 1083.46 0.57 555.87 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 324.24 0.7054000 17.60 0.5124829 2.09 16.79 0.93 1082.73 0.57 556.90 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 322.67 0.7054000 17.61 0.5124829 2.09 16.79 0.93 1082.00 0.57 557.94 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 321.07 0.7054000 17.62 0.5124829 2.09 16.79 0.93 1081.27 0.57 558.98 1.19 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 319.46 0.7054000 17.63 0.5124829 2.09 16.79 0.93 1080.54 0.57 560.03 1.18 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 317.83 0.7054000 17.64 0.5124829 2.09 16.79 0.93 1079.81 0.57 561.09 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.12 5.80 0.90 0.30 316.18 0.7054000 17.66 0.5124829 2.10 16.79 0.93 1079.08 0.57 562.16 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 314.51 0.7054000 17.67 0.5124829 2.10 16.79 0.93 1078.36 0.57 563.23 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 312.82 0.7054000 17.68 0.5124829 2.10 16.79 0.93 1077.63 0.57 564.31 1.18 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 311.12 0.7054000 17.69 0.5124829 2.10 16.79 0.93 1076.90 0.58 565.40 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 309.39 0.7054000 17.71 0.5124829 2.10 16.79 0.93 1076.17 0.58 566.49 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 307.65 0.7054000 17.72 0.5124829 2.11 16.79 0.93 1075.44 0.58 567.59 1.17 0.00 0.00 0.00 0.89 0.13 0.00 0.14 5.80 0.89 0.30 305.88 0.7054001 17.73 0.5124829 2.11 16.79 0.93 1074.71 0.58 568.70 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 304.10 0.7054001 17.75 0.5124829 2.11 16.79 0.92 1073.98 0.58 569.82 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 302.30 0.7054001 17.76 0.5124829 2.11 16.79 0.92 1073.26 0.58 570.94 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 300.48 0.7054001 17.78 0.5124829 2.11 16.79 0.92 1072.53 0.58 572.08 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.15 5.80 0.89 0.30 298.64 0.7054001 17.79 0.5124829 2.12 16.79 0.92 1071.80 0.58 573.22 1.16 0.00 0.00 0.00 0.89 0.15 0.00 0.15 5.80 0.89 0.30 296.78 0.7054001 17.81 0.5124829 2.12 16.79 0.92 1071.07 0.58 574.37 1.16 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 294.90 0.7054001 17.82 0.5124829 2.12 16.79 0.92 1070.34 0.58 575.52 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 293.00 0.7054001 17.84 0.5124829 2.12 16.79 0.92 1069.61 0.58 576.68 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.16 5.80 0.88 0.30 291.09 0.7054001 17.85 0.5124829 2.13 16.79 0.92 1068.88 0.58 577.86 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 289.16 0.7054001 17.87 0.5124829 2.13 16.79 0.92 1068.16 0.58 579.04 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 287.20 0.7054001 17.88 0.5124829 2.13 16.79 0.92 1067.43 0.59 580.22 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.16 5.80 0.87 0.30 285.23 0.7054001 17.90 0.5124829 2.13 16.79 0.92 1066.70 0.59 581.42 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.17 5.80 0.87 0.30 283.24 0.7054001 17.92 0.5124829 2.14 16.79 0.92 1065.97 0.59 582.63 1.14 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 281.24 0.7054001 17.93 0.5124829 2.14 16.79 0.92 1065.24 0.59 583.84 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 279.21 0.7054001 17.95 0.5124829 2.14 16.79 0.92 1064.51 0.59 585.06 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.18 5.80 0.87 0.30 277.17 0.7054001 17.97 0.5124829 2.14 16.79 0.92 1063.78 0.59 586.29 1.13 0.00 0.00 0.00 0.86 0.17 0.00 0.18 5.80 0.86 0.30 275.11 0.7054001 17.99 0.5124828 2.15 16.79 0.92 1063.06 0.59 587.53 1.13 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 273.04 0.7054001 18.01 0.5124828 2.15 16.79 0.92 1062.33 0.59 588.78 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 270.94 0.7054001 18.02 0.5124828 2.15 16.79 0.92 1061.60 0.59 590.03 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.19 5.80 0.86 0.30 268.83 0.7054001 18.04 0.5124828 2.15 16.79 0.92 1060.87 0.59 591.30 1.12 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 266.70 0.7054001 18.06 0.5124828 2.16 16.79 0.92 1060.14 0.59 592.57 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 264.56 0.7054001 18.08 0.5124828 2.16 16.79 0.91 1059.41 0.60 593.86 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 262.40 0.7054001 18.10 0.5124828 2.16 16.79 0.91 1058.68 0.60 595.15 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 260.22 0.7054001 18.12 0.5124828 2.17 16.79 0.91 1057.96 0.60 596.45 1.11 0.00 0.00 0.00 0.85 0.20 0.00 0.20 5.80 0.85 0.30 258.03 0.7054001 18.14 0.5124828 2.17 16.79 0.91 1057.23 0.60 597.76 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.20 5.80 0.84 0.30 255.82 0.7054001 18.16 0.5124828 2.17 16.79 0.91 1056.50 0.60 599.08 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.21 5.80 0.84 0.30 253.60 0.7054002 18.18 0.5124828 2.18 16.79 0.91 1055.77 0.60 600.41 1.10 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 251.36 0.7054002 18.21 0.5124828 2.18 16.79 0.91 1055.04 0.60 601.74 1.09 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 249.10 0.7054002 18.23 0.5124828 2.18 16.79 0.91 1054.31 0.60 603.09 1.09 0.00 0.00 0.00 0.83 0.21 0.00 0.22 5.80 0.83 0.30 246.84 0.7054002 18.25 0.5124827 2.18 16.79 0.91 1053.58 0.60 604.45 1.09 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 244.56 0.7054002 18.27 0.5124827 2.19 16.79 0.91 1052.86 0.60 605.81 1.08 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 242.26 0.7054002 18.30 0.5124827 2.19 16.79 0.91 1052.13 0.60 607.19 1.08 0.00 0.00 0.00 0.82 0.22 0.00 0.23 5.80 0.82 0.30 239.95 0.7054002 18.32 0.5124827 2.20 16.79 0.91 1051.40 0.61 608.57 1.08 0.00 0.00 0.00 0.82 0.23 0.00 0.23 5.80 0.82 0.30 237.63 0.7054002 18.34 0.5124827 2.20 16.79 0.91 1050.67 0.61 609.96 1.07 0.00 0.00 0.00 0.82 0.23 0.00 0.24 5.80 0.82 0.30 235.30 0.7054002 18.37 0.5124827 2.20 16.79 0.91 1049.94 0.61 611.37 1.07 0.00 0.00 0.00 0.82 0.24 0.00 0.24 5.80 0.82 0.30 232.95 0.7054002 18.39 0.5124827 2.21 16.79 0.91 1049.21 0.61 612.78 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.24 5.80 0.81 0.30 230.60 0.7054003 18.42 0.5124827 2.21 16.79 0.91 1048.48 0.61 614.20 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.25 5.80 0.81 0.30 228.23 0.7054003 18.44 0.5124826 2.21 16.79 0.91 1047.76 0.61 615.63 1.06 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 225.85 0.7054003 18.47 0.5124826 2.22 16.79 0.91 1047.03 0.61 617.07 1.05 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 223.46 0.7054003 18.50 0.5124826 2.22 16.79 0.91 1046.30 0.61 618.52 1.05 0.00 0.00 0.00 0.80 0.25 0.00 0.26 5.80 0.80 0.30 221.06 0.7054003 18.52 0.5124826 2.23 16.79 0.91 1045.57 0.61 619.98 1.05 0.00 0.00 0.00 0.80 0.26 0.00 0.26 5.80 0.80 0.30 218.65 0.7054003 18.55 0.5124826 2.23 16.79 0.90 1044.84 0.61 621.45 1.04 0.00 0.00 0.00 0.80 0.26 0.00 0.27 5.80 0.80 0.30 216.23 0.7054004 18.58 0.5124826 2.23 16.79 0.90 1044.11 0.61 622.93 1.04 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 213.80 0.7054004 18.61 0.5124825 2.24 16.79 0.90 1043.38 0.62 624.42 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 211.37 0.7054004 18.63 0.5124825 2.24 16.79 0.90 1042.66 0.62 625.92 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.28 5.80 0.79 0.30 208.93 0.7054004 18.66 0.5124825 2.25 16.79 0.90 1041.93 0.62 627.43 1.03 0.00 0.00 0.00 0.78 0.28 0.00 0.28 5.80 0.78 0.30 206.48 0.7054004 18.69 0.5124825 2.25 16.79 0.90 1041.20 0.62 628.95 1.02 0.00 0.00 0.00 0.78 0.28 0.00 0.29 5.80 0.78 0.30 204.02 0.7054005 18.72 0.5124824 2.26 16.79 0.90 1040.47 0.62 630.47 1.02 0.00 0.00 0.00 0.78 0.29 0.00 0.29 5.80 0.78 0.30 201.56 0.7054005 18.75 0.5124824 2.26 16.79 0.90 1039.74 0.62 632.01 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.29 5.80 0.77 0.30 199.10 0.7054005 18.78 0.5124824 2.27 16.79 0.90 1039.01 0.62 633.56 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.30 5.80 0.77 0.30 196.63 0.7054006 18.82 0.5124823 2.27 16.79 0.90 1038.28 0.62 635.11 1.01 0.00 0.00 0.00 0.77 0.30 0.00 0.30 5.80 0.77 0.30 194.15 0.7054006 18.85 0.5124823 2.27 16.79 0.90 1037.56 0.62 636.68 1.00 0.00 0.00 0.00 0.76 0.30 0.00 0.31 5.80 0.76 0.30 191.67 0.7054006 18.88 0.5124823 2.28 16.79 0.90 1036.83 0.63 638.25 1.00 0.00 0.00 0.00 0.76 0.31 0.00 0.31 5.80 0.76 0.30 189.19 0.7054007 18.91 0.5124822 2.28 16.79 0.90 1036.10 0.63 639.84 0.99 0.00 0.00 0.00 0.76 0.31 0.00 0.32 5.80 0.76 0.30 186.71 0.7054007 18.95 0.5124822 2.29 16.79

145 0.90 1035.37 0.63 641.43 0.99 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 184.23 0.7054008 18.98 0.5124822 2.30 16.79 0.90 1034.64 0.63 643.03 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 181.74 0.7054008 19.02 0.5124821 2.30 16.79 0.90 1033.91 0.63 644.65 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.33 5.80 0.75 0.30 179.25 0.7054009 19.05 0.5124821 2.31 16.79 0.90 1033.18 0.63 646.27 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.33 5.80 0.74 0.30 176.77 0.7054009 19.09 0.5124820 2.31 16.79 0.90 1032.46 0.63 647.90 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.34 5.80 0.74 0.30 174.28 0.7054010 19.12 0.5124820 2.32 16.79 0.90 1031.73 0.63 649.54 0.97 0.00 0.00 0.00 0.74 0.34 0.00 0.34 5.80 0.74 0.30 171.80 0.7054010 19.16 0.5124819 2.32 16.79 0.90 1031.00 0.63 651.19 0.96 0.00 0.00 0.00 0.73 0.34 0.00 0.35 5.80 0.73 0.30 169.32 0.7054011 19.20 0.5124819 2.33 16.79 0.89 1030.27 0.64 652.85 0.96 0.00 0.00 0.00 0.73 0.35 0.00 0.35 5.80 0.73 0.30 166.84 0.7054012 19.24 0.5124818 2.33 16.79 0.89 1029.54 0.64 654.51 0.95 0.00 0.00 0.00 0.73 0.35 0.00 0.36 5.80 0.73 0.30 164.36 0.7054013 19.28 0.5124818 2.34 16.79 0.89 1028.81 0.64 656.19 0.95 0.00 0.00 0.00 0.72 0.36 0.00 0.36 5.80 0.72 0.30 161.89 0.7054014 19.32 0.5124817 2.35 16.79 0.89 1028.08 0.64 657.87 0.94 0.00 0.00 0.00 0.72 0.36 0.00 0.37 5.80 0.72 0.30 159.42 0.7054015 19.36 0.5124816 2.35 16.79 0.89 1027.36 0.64 659.56 0.94 0.00 0.00 0.00 0.72 0.37 0.00 0.37 5.80 0.72 0.30 156.96 0.7054016 19.40 0.5124816 2.36 16.79 0.89 1026.63 0.64 661.27 0.93 0.00 0.00 0.00 0.71 0.37 0.00 0.38 5.80 0.71 0.30 154.51 0.7054017 19.44 0.5124815 2.36 16.79 0.89 1025.90 0.64 662.98 0.93 0.00 0.00 0.00 0.71 0.38 0.00 0.38 5.80 0.71 0.30 152.06 0.7054018 19.48 0.5124814 2.37 16.79 0.89 1025.17 0.64 664.69 0.92 0.00 0.00 0.00 0.70 0.38 0.00 0.39 5.80 0.70 0.30 149.62 0.7054019 19.52 0.5124813 2.38 16.79 0.89 1024.44 0.64 666.42 0.92 0.00 0.00 0.00 0.70 0.39 0.00 0.39 5.80 0.70 0.30 147.19 0.7054021 19.57 0.5124812 2.38 16.79 0.89 1023.71 0.65 668.15 0.91 0.00 0.00 0.00 0.70 0.39 0.00 0.40 5.80 0.70 0.30 144.76 0.7054022 19.61 0.5124811 2.39 16.79 0.89 1022.98 0.65 669.90 0.91 0.00 0.00 0.00 0.69 0.40 0.00 0.40 5.80 0.69 0.30 142.35 0.7054024 19.66 0.5124810 2.40 16.79 0.89 1022.26 0.65 671.65 0.90 0.00 0.00 0.00 0.69 0.40 0.00 0.41 5.80 0.69 0.30 139.94 0.7054025 19.70 0.5124809 2.41 16.79 0.89 1021.53 0.65 673.40 0.90 0.00 0.00 0.00 0.68 0.41 0.00 0.41 5.80 0.68 0.30 137.55 0.7054027 19.75 0.5124808 2.41 16.79 0.89 1020.80 0.65 675.17 0.89 0.00 0.00 0.00 0.68 0.41 0.00 0.42 5.80 0.68 0.30 135.17 0.7054029 19.80 0.5124807 2.42 16.79 0.89 1020.07 0.65 676.94 0.89 0.00 0.00 0.00 0.68 0.42 0.00 0.42 5.80 0.68 0.30 132.80 0.7054031 19.84 0.5124805 2.43 16.79 0.89 1019.34 0.65 678.72 0.88 0.00 0.00 0.00 0.67 0.42 0.00 0.43 5.80 0.67 0.30 130.44 0.7054034 19.89 0.5124804 2.43 16.79 0.89 1018.61 0.65 680.51 0.88 0.00 0.00 0.00 0.67 0.43 0.00 0.43 5.80 0.67 0.30 128.09 0.7054036 19.94 0.5124803 2.44 16.79 0.89 1017.88 0.66 682.30 0.87 0.00 0.00 0.00 0.66 0.43 0.00 0.44 5.80 0.66 0.30 125.76 0.7054039 19.99 0.5124801 2.45 16.79 0.89 1017.16 0.66 684.11 0.87 0.00 0.00 0.00 0.66 0.44 0.00 0.44 5.80 0.66 0.30 123.45 0.7054042 20.04 0.5124799 2.46 16.79 0.89 1016.43 0.66 685.91 0.86 0.00 0.00 0.00 0.66 0.44 0.00 0.45 5.80 0.66 0.30 121.15 0.7054046 20.10 0.5124798 2.47 16.79 0.88 1015.70 0.66 687.73 0.85 0.00 0.00 0.00 0.65 0.45 0.00 0.45 5.80 0.65 0.30 118.86 0.7054049 20.15 0.5124796 2.47 16.79 0.88 1014.97 0.66 689.55 0.85 0.00 0.00 0.00 0.65 0.46 0.00 0.46 5.80 0.65 0.30 116.59 0.7054053 20.20 0.5124794 2.48 16.79 0.88 1014.24 0.66 691.38 0.84 0.00 0.00 0.00 0.64 0.46 0.00 0.46 5.80 0.64 0.30 114.34 0.7054057 20.26 0.5124792 2.49 16.79 0.88 1013.51 0.66 693.21 0.84 0.00 0.00 0.00 0.64 0.47 0.00 0.47 5.79 0.64 0.30 112.11 0.7054062 20.31 0.5124790 2.50 16.79 0.88 1012.78 0.66 695.06 0.83 0.00 0.00 0.00 0.63 0.47 0.00 0.48 5.79 0.63 0.30 109.89 0.7054067 20.37 0.5124787 2.51 16.79 0.88 1012.06 0.67 696.91 0.83 0.00 0.00 0.00 0.63 0.48 0.00 0.48 5.79 0.63 0.30 107.69 0.7054072 20.43 0.5124785 2.52 16.79 0.88 1011.33 0.67 698.77 0.82 0.00 0.00 0.00 0.63 0.48 0.00 0.49 5.79 0.63 0.30 105.51 0.7054078 20.49 0.5124782 2.53 16.79 0.88 1010.60 0.67 700.65 0.82 0.00 0.00 0.00 0.62 0.49 0.00 0.49 5.79 0.62 0.30 103.36 0.7054084 20.55 0.5124779 2.54 16.79 0.88 1009.87 0.67 702.54 0.81 0.00 0.00 0.00 0.62 0.49 0.00 0.50 5.79 0.62 0.30 101.22 0.7054091 20.61 0.5124776 2.55 16.80 0.88 1009.14 0.67 704.45 0.81 0.00 0.00 0.00 0.61 0.50 0.00 0.50 5.79 0.61 0.30 99.10 0.7054099 20.67 0.5124773 2.56 16.80 0.88 1008.41 0.67 706.39 0.80 0.00 0.00 0.00 0.61 0.51 0.00 0.51 5.79 0.61 0.30 97.00 0.7054108 20.73 0.5124769 2.57 16.80 0.88 1007.68 0.67 708.37 0.79 0.00 0.00 0.00 0.60 0.51 0.00 0.52 5.79 0.60 0.30 94.92 0.7054117 20.79 0.5124766 2.58 16.80 0.88 1006.96 0.67 710.40 0.79 0.00 0.00 0.00 0.60 0.52 0.00 0.52 5.79 0.60 0.30 92.87 0.7054128 20.86 0.5124761 2.59 16.80 0.88 1006.23 0.68 712.51 0.78 0.00 0.00 0.00 0.60 0.52 0.01 0.53 5.79 0.60 0.30 90.84 0.7054139 20.93 0.5124757 2.60 16.80 0.88 1005.50 0.68 714.72 0.78 0.00 0.00 0.00 0.59 0.53 0.01 0.54 5.79 0.59 0.30 88.82 0.7054153 21.00 0.5124752 2.61 16.80 0.88 1004.77 0.68 717.07 0.78 0.00 0.00 0.00 0.59 0.54 0.01 0.54 5.79 0.59 0.31 86.83 0.7054169 21.07 0.5124746 2.62 16.80 0.88 1004.04 0.68 719.59 0.77 0.00 0.00 0.00 0.58 0.54 0.01 0.55 5.79 0.58 0.31 84.87 0.7054188 21.14 0.5124740 2.63 16.80 0.88 1003.31 0.68 722.33 0.77 0.00 0.00 0.00 0.58 0.55 0.01 0.56 5.79 0.58 0.31 82.92 0.7054210 21.22 0.5124732 2.64 16.80 0.88 1002.58 0.69 725.33 0.77 0.00 0.00 0.00 0.57 0.55 0.01 0.57 5.79 0.57 0.32 81.00 0.7054237 21.30 0.5124723 2.65 16.80 0.88 1001.86 0.69 728.63 0.76 0.00 0.00 0.00 0.57 0.56 0.02 0.58 5.78 0.57 0.33 79.09 0.7054271 21.38 0.5124712 2.67 16.80 0.87 1001.13 0.69 732.25 0.76 0.00 0.00 0.00 0.56 0.56 0.02 0.59 5.78 0.56 0.33 77.21 0.7054313 21.47 0.5124699 2.68 16.80 0.87 1000.40 0.69 736.19 0.76 0.00 0.00 0.00 0.56 0.57 0.02 0.60 5.78 0.56 0.34 75.35 0.7054364 21.57 0.5124684 2.70 16.80 0.87 999.67 0.70 740.42 0.76 0.00 0.00 0.00 0.55 0.58 0.03 0.61 5.78 0.55 0.35 73.52 0.7054428 21.67 0.5124665 2.71 16.81 0.87 998.94 0.70 744.89 0.76 0.00 0.00 0.00 0.55 0.58 0.04 0.62 5.77 0.55 0.37 71.71 0.7054506 21.77 0.5124643 2.73 16.81 0.87 998.21 0.70 749.53 0.76 0.00 0.00 0.00 0.55 0.59 0.04 0.63 5.77 0.55 0.38 69.92 0.7054601 21.88 0.5124617 2.74 16.81 0.87 997.48 0.71 754.26 0.77 0.00 0.00 0.00 0.54 0.60 0.05 0.64 5.77 0.54 0.39 68.16 0.7054714 22.00 0.5124587 2.76 16.81 0.87 996.75 0.71 758.97 0.77 0.00 0.01 0.01 0.54 0.60 0.05 0.66 5.76 0.54 0.40 66.43 0.7054846 22.13 0.5124553 2.78 16.82 0.87 996.03 0.71 763.59 0.77 0.00 0.01 0.01 0.53 0.61 0.06 0.67 5.76 0.53 0.42 64.73 0.7054998 22.25 0.5124515 2.80 16.82 0.87 995.30 0.71 768.04 0.77 0.00 0.01 0.01 0.53 0.62 0.06 0.68 5.75 0.53 0.43 63.05 0.7055170 22.39 0.5124474 2.83 16.82 0.87 994.57 0.72 772.29 0.77 0.00 0.01 0.01 0.52 0.62 0.07 0.69 5.74 0.52 0.44 61.41 0.7055361 22.52 0.5124430 2.85 16.83 0.87 993.84 0.72 776.31 0.77 0.01 0.01 0.01 0.52 0.63 0.07 0.70 5.74 0.52 0.45 59.80 0.7055570 22.66 0.5124383 2.87 16.83 0.87 993.11 0.72 780.08 0.77 0.01 0.01 0.01 0.51 0.64 0.08 0.71 5.73 0.51 0.46 58.22 0.7055796 22.80 0.5124334 2.90 16.83 0.87 992.38 0.73 783.60 0.76 0.01 0.01 0.01 0.51 0.64 0.08 0.72 5.72 0.51 0.46 56.67 0.7056039 22.95 0.5124283 2.92 16.84 0.87 991.65 0.73 786.90 0.76 0.01 0.01 0.01 0.50 0.65 0.08 0.73 5.71 0.50 0.47 55.16 0.7056297 23.09 0.5124231 2.95 16.84 0.87 990.93 0.73 789.99 0.76 0.01 0.01 0.01 0.50 0.66 0.09 0.74 5.70 0.50 0.48 53.67 0.7056571 23.24 0.5124178 2.98 16.85 0.87 990.20 0.73 792.89 0.75 0.01 0.02 0.02 0.49 0.66 0.09 0.75 5.70 0.49 0.48 52.22 0.7056862 23.39 0.5124124 3.00 16.85 0.87 989.47 0.73 795.62 0.75 0.01 0.02 0.02 0.49 0.67 0.09 0.76 5.69 0.49 0.48 50.80 0.7057169 23.55 0.5124068 3.03 16.86 0.87 988.74 0.74 798.20 0.75 0.01 0.02 0.02 0.49 0.68 0.09 0.77 5.68 0.49 0.49 49.41 0.7057493 23.70 0.5124012 3.06 16.86 0.87 988.01 0.74 800.66 0.74 0.01 0.02 0.02 0.48 0.68 0.09 0.77 5.67 0.48 0.49 48.05 0.7057838 23.86 0.5123954 3.09 16.87 0.87 987.28 0.74 803.02 0.74 0.01 0.02 0.02 0.48 0.69 0.09 0.78 5.66 0.48 0.49 46.72 0.7058203 24.02 0.5123895 3.12 16.87 0.86 986.55 0.74 805.28 0.73 0.01 0.02 0.02 0.47 0.70 0.09 0.79 5.65 0.47 0.49 45.42 0.7058591 24.18 0.5123835 3.15 16.88 0.86 985.83 0.74 807.46 0.73 0.01 0.02 0.02 0.47 0.70 0.09 0.80 5.64 0.47 0.49 44.15 0.7059004 24.35 0.5123773 3.18 16.88 0.86 985.10 0.74 809.58 0.72 0.01 0.02 0.02 0.46 0.71 0.09 0.81 5.63 0.46 0.49 42.92 0.7059445 24.52 0.5123710 3.21 16.89 0.86 984.37 0.74 811.63 0.72 0.01 0.03 0.03 0.46 0.72 0.09 0.81 5.62 0.46 0.50 41.71 0.7059916 24.69 0.5123644 3.24 16.89 0.86 983.64 0.75 813.63 0.71 0.02 0.03 0.03 0.45 0.72 0.10 0.82 5.61 0.45 0.50 40.53 0.7060419 24.87 0.5123578 3.28 16.90 0.86 982.91 0.75 815.59 0.71 0.02 0.03 0.03 0.45 0.73 0.10 0.83 5.59 0.45 0.50 39.38 0.7060958 25.05 0.5123509 3.31 16.90 0.86 982.18 0.75 817.51 0.70 0.02 0.03 0.03 0.44 0.74 0.10 0.83 5.58 0.44 0.50 38.27 0.7061535 25.23 0.5123438 3.35 16.91 0.86 981.45 0.75 819.39 0.70 0.02 0.03 0.03 0.44 0.75 0.10 0.84 5.57 0.44 0.50 37.18 0.7062153 25.42 0.5123365 3.38 16.92 0.86 980.73 0.75 821.24 0.69 0.02 0.03 0.03 0.44 0.75 0.10 0.85 5.55 0.44 0.50 36.12 0.7062815 25.62 0.5123290 3.42 16.92 0.86 980.00 0.75 823.05 0.69 0.02 0.04 0.04 0.43 0.76 0.10 0.85 5.54 0.43 0.50 35.09 0.7063524 25.82 0.5123213 3.46 16.93 0.86 979.27 0.75 824.84 0.68 0.02 0.04 0.04 0.43 0.77 0.10 0.86 5.53 0.43 0.50 34.09 0.7064283 26.02 0.5123134 3.50 16.94 0.86 978.54 0.75 826.60 0.68 0.02 0.04 0.04 0.42 0.77 0.10 0.87 5.51 0.42 0.50 33.11 0.7065095 26.23 0.5123052 3.54 16.94 0.86 977.81 0.76 828.33 0.67 0.02 0.04 0.04 0.42 0.78 0.10 0.88 5.49 0.42 0.50 32.17 0.7065963 26.44 0.5122969 3.58 16.95 0.86 977.08 0.76 830.04 0.67 0.02 0.04 0.04 0.41 0.79 0.10 0.88 5.48 0.41 0.50 31.26 0.7066890 26.66 0.5122884 3.63 16.95 0.86 976.35 0.76 831.73 0.66 0.03 0.05 0.05 0.41 0.79 0.10 0.89 5.46 0.41 0.50 30.37 0.7067880 26.88 0.5122796 3.67 16.96 0.86 975.63 0.76 833.39 0.66 0.03 0.05 0.05 0.40 0.80 0.10 0.90 5.44 0.40 0.50 29.51 0.7068935 27.11 0.5122707 3.71 16.97 0.86 974.90 0.76 835.03 0.66 0.03 0.05 0.05 0.40 0.81 0.10 0.90 5.43 0.40 0.50 28.68 0.7070058 27.34 0.5122615 3.76 16.98 0.86 974.17 0.76 836.65 0.65 0.03 0.05 0.05 0.39 0.81 0.10 0.91 5.41 0.39 0.50 27.87 0.7071254 27.58 0.5122522 3.81 16.98 0.86 973.44 0.76 838.24 0.65 0.03 0.06 0.06 0.39 0.82 0.10 0.92 5.39 0.39 0.50 27.10 0.7072523 27.82 0.5122427 3.86 16.99 0.86 972.71 0.76 839.82 0.64 0.03 0.06 0.06 0.39 0.83 0.10 0.92 5.37 0.39 0.50 26.35 0.7073870 28.07 0.5122330 3.91 17.00 0.85 971.98 0.76 841.37 0.64 0.03 0.06 0.06 0.38 0.83 0.10 0.93 5.35 0.38 0.50 25.62 0.7075296 28.32 0.5122232 3.96 17.00 0.85 971.25 0.77 842.90 0.64 0.04 0.06 0.06 0.38 0.84 0.10 0.94 5.33 0.38 0.50 24.92 0.7076805 28.58 0.5122132 4.01 17.01 0.85 970.53 0.77 844.41 0.63 0.04 0.07 0.07 0.37 0.85 0.10 0.94 5.30 0.37 0.50 24.25 0.7078398 28.84 0.5122031 4.06 17.02 0.85 969.80 0.77 845.89 0.63 0.04 0.07 0.07 0.37 0.85 0.10 0.95 5.28 0.37 0.50 23.60 0.7080077 29.11 0.5121928 4.12 17.03 0.85 969.07 0.77 847.36 0.62 0.04 0.07 0.07 0.36 0.86 0.10 0.95 5.26 0.36 0.50 22.98 0.7081845 29.38 0.5121824 4.17 17.03 0.85 968.34 0.77 848.81 0.62 0.04 0.07 0.07 0.36 0.86 0.10 0.96 5.23 0.36 0.50 22.38 0.7083702 29.66 0.5121719 4.23 17.04 0.85 967.61 0.77 850.23 0.62 0.04 0.08 0.08 0.36 0.87 0.10 0.97 5.21 0.36 0.50 21.81 0.7085651 29.94 0.5121613 4.29 17.05 0.85 966.88 0.77 851.64 0.61 0.05 0.08 0.08 0.35 0.88 0.10 0.97 5.19 0.35 0.50 21.26 0.7087691 30.22 0.5121507 4.35 17.06 0.85 966.15 0.77 853.02 0.61 0.05 0.08 0.08 0.35 0.88 0.10 0.98 5.16 0.35 0.50 20.73 0.7089822 30.51 0.5121399 4.41 17.06 0.85 965.43 0.77 854.39 0.61 0.05 0.09 0.09 0.34 0.89 0.10 0.99 5.13 0.34 0.50 20.23 0.7092046 30.80 0.5121291 4.47 17.07 0.85 964.70 0.77 855.74 0.61 0.05 0.09 0.09 0.34 0.90 0.10 0.99 5.11 0.34 0.50 19.74 0.7094362 31.10 0.5121182 4.53 17.08 0.85 963.97 0.78 857.06 0.60 0.05 0.09 0.09 0.33 0.90 0.10 1.00 5.08 0.33 0.50 19.28 0.7096768 31.40 0.5121073 4.59 17.09

146 0.85 963.24 0.78 858.37 0.60 0.05 0.10 0.10 0.33 0.91 0.10 1.00 5.05 0.33 0.50 18.84 0.7099264 31.70 0.5120964 4.65 17.09 0.85 962.51 0.78 859.66 0.60 0.06 0.10 0.10 0.33 0.91 0.10 1.01 5.03 0.33 0.50 18.42 0.7101847 32.00 0.5120854 4.72 17.10 0.85 961.78 0.78 860.93 0.59 0.06 0.10 0.10 0.32 0.92 0.10 1.02 5.00 0.32 0.50 18.02 0.7104516 32.31 0.5120744 4.78 17.11 0.85 961.05 0.78 862.19 0.59 0.06 0.11 0.11 0.32 0.93 0.10 1.02 4.97 0.32 0.50 17.64 0.7107267 32.62 0.5120634 4.85 17.12 0.85 960.33 0.78 863.42 0.59 0.06 0.11 0.11 0.31 0.93 0.10 1.03 4.94 0.31 0.50 17.28 0.7110098 32.93 0.5120525 4.91 17.12 0.85 959.60 0.78 864.64 0.59 0.07 0.11 0.11 0.31 0.94 0.10 1.03 4.91 0.31 0.50 16.94 0.7113004 33.25 0.5120415 4.98 17.13 0.85 958.87 0.78 865.83 0.59 0.07 0.12 0.12 0.31 0.94 0.10 1.04 4.88 0.31 0.50 16.61 0.7115982 33.57 0.5120306 5.05 17.14 0.85 958.14 0.78 867.02 0.58 0.07 0.12 0.12 0.30 0.95 0.10 1.05 4.85 0.30 0.50 16.31 0.7119027 33.88 0.5120197 5.11 17.15 0.84 957.41 0.78 868.18 0.58 0.07 0.13 0.13 0.30 0.96 0.10 1.05 4.82 0.30 0.50 16.02 0.7122134 34.21 0.5120089 5.18 17.15 0.84 956.68 0.78 869.33 0.58 0.07 0.13 0.13 0.30 0.96 0.10 1.06 4.79 0.30 0.50 15.74 0.7125298 34.53 0.5119981 5.25 17.16 0.84 955.95 0.78 870.46 0.58 0.08 0.13 0.13 0.29 0.97 0.10 1.06 4.75 0.29 0.50 15.48 0.7128513 34.85 0.5119874 5.32 17.17 0.84 955.23 0.79 871.58 0.58 0.08 0.14 0.14 0.29 0.97 0.10 1.07 4.72 0.29 0.50 15.24 0.7131774 35.17 0.5119768 5.39 17.17 0.84 954.50 0.79 872.68 0.58 0.08 0.14 0.14 0.28 0.98 0.10 1.08 4.69 0.28 0.50 15.01 0.7135073 35.50 0.5119662 5.46 17.18 0.84 953.77 0.79 873.76 0.57 0.08 0.15 0.15 0.28 0.98 0.10 1.08 4.66 0.28 0.50 14.80 0.7138405 35.82 0.5119557 5.53 17.19 0.84 953.04 0.79 874.83 0.57 0.09 0.15 0.15 0.28 0.99 0.10 1.09 4.63 0.28 0.50 14.60 0.7141764 36.15 0.5119453 5.60 17.19 0.84 952.31 0.79 875.89 0.57 0.09 0.15 0.15 0.27 1.00 0.10 1.09 4.59 0.27 0.50 14.42 0.7145142 36.47 0.5119350 5.67 17.20 0.84 951.58 0.79 876.92 0.57 0.09 0.16 0.16 0.27 1.00 0.10 1.10 4.56 0.27 0.50 14.24 0.7148534 36.80 0.5119248 5.74 17.21 0.84 950.85 0.79 877.95 0.57 0.09 0.16 0.16 0.27 1.01 0.10 1.10 4.53 0.27 0.50 14.08 0.7151932 37.12 0.5119147 5.81 17.21 0.84 950.13 0.79 878.96 0.57 0.10 0.17 0.17 0.26 1.01 0.10 1.11 4.49 0.26 0.50 13.93 0.7155330 37.45 0.5119047 5.88 17.22 0.84 949.40 0.79 879.96 0.57 0.10 0.17 0.17 0.26 1.02 0.10 1.11 4.46 0.26 0.50 13.80 0.7158722 37.77 0.5118948 5.95 17.22 0.84 948.67 0.79 880.94 0.57 0.10 0.18 0.18 0.25 1.02 0.10 1.12 4.43 0.25 0.50 13.67 0.7162102 38.10 0.5118850 6.02 17.23 0.84 947.94 0.79 881.91 0.57 0.10 0.18 0.18 0.25 1.03 0.10 1.12 4.39 0.25 0.50 13.56 0.7165463 38.42 0.5118753 6.09 17.24 0.84 947.21 0.79 882.87 0.56 0.11 0.19 0.19 0.25 1.03 0.10 1.13 4.36 0.25 0.50 13.46 0.7168799 38.74 0.5118658 6.16 17.24 0.84 946.48 0.79 883.82 0.56 0.11 0.19 0.19 0.24 1.04 0.10 1.13 4.33 0.24 0.50 13.36 0.7172106 39.06 0.5118564 6.23 17.25 0.84 945.75 0.79 884.75 0.56 0.11 0.20 0.20 0.24 1.04 0.10 1.14 4.29 0.24 0.50 13.28 0.7175379 39.37 0.5118471 6.30 17.25 0.84 945.03 0.80 885.67 0.56 0.11 0.20 0.20 0.24 1.05 0.10 1.14 4.26 0.24 0.50 13.20 0.7178611 39.69 0.5118379 6.37 17.26 0.84 944.30 0.80 886.58 0.56 0.12 0.20 0.20 0.23 1.05 0.10 1.15 4.23 0.23 0.50 13.14 0.7181799 40.00 0.5118288 6.44 17.26 0.84 943.57 0.80 887.48 0.56 0.12 0.21 0.21 0.23 1.06 0.10 1.15 4.19 0.23 0.50 13.08 0.7184939 40.31 0.5118199 6.51 17.27 0.83 942.84 0.80 888.36 0.56 0.12 0.21 0.21 0.23 1.06 0.10 1.16 4.16 0.23 0.50 13.03 0.7188026 40.62 0.5118111 6.58 17.27 0.83 942.11 0.80 889.24 0.56 0.12 0.22 0.22 0.22 1.07 0.10 1.16 4.13 0.22 0.50 12.99 0.7191058 40.92 0.5118024 6.64 17.28 0.83 941.38 0.80 890.10 0.56 0.13 0.22 0.22 0.22 1.07 0.10 1.17 4.09 0.22 0.50 12.96 0.7194032 41.23 0.5117939 6.71 17.28 0.83 940.65 0.80 890.95 0.56 0.13 0.23 0.23 0.22 1.08 0.10 1.17 4.06 0.22 0.50 12.93 0.7196944 41.53 0.5117855 6.78 17.29 0.83 939.93 0.80 891.80 0.56 0.13 0.23 0.23 0.21 1.08 0.10 1.18 4.03 0.21 0.50 12.91 0.7199792 41.82 0.5117772 6.84 17.29 0.83 939.20 0.80 892.63 0.56 0.14 0.24 0.24 0.21 1.09 0.10 1.18 4.00 0.21 0.50 12.90 0.7202575 42.12 0.5117690 6.91 17.30 0.83 938.47 0.80 893.45 0.56 0.14 0.24 0.24 0.21 1.09 0.10 1.19 3.96 0.21 0.50 12.89 0.7205291 42.41 0.5117610 6.97 17.30 0.83 937.74 0.80 894.27 0.56 0.14 0.25 0.25 0.21 1.10 0.10 1.19 3.93 0.21 0.50 12.90 0.7207939 42.70 0.5117531 7.04 17.31 0.83 937.01 0.80 895.07 0.57 0.14 0.25 0.25 0.20 1.10 0.10 1.20 3.90 0.20 0.50 12.90 0.7210518 42.98 0.5117453 7.10 17.31 0.83 936.28 0.80 895.86 0.57 0.15 0.26 0.26 0.20 1.10 0.10 1.20 3.87 0.20 0.50 12.91 0.7213027 43.26 0.5117377 7.17 17.32 0.83 935.55 0.80 896.65 0.57 0.15 0.26 0.26 0.20 1.11 0.10 1.21 3.83 0.20 0.50 12.93 0.7215465 43.54 0.5117302 7.23 17.32 0.83 934.83 0.80 897.43 0.57 0.15 0.27 0.27 0.19 1.11 0.10 1.21 3.80 0.19 0.50 12.96 0.7217834 43.82 0.5117228 7.29 17.32 0.83 934.10 0.80 898.19 0.57 0.16 0.27 0.27 0.19 1.12 0.10 1.21 3.77 0.19 0.50 12.98 0.7220132 44.09 0.5117155 7.35 17.33 0.83 933.37 0.80 898.95 0.57 0.16 0.28 0.28 0.19 1.12 0.10 1.22 3.74 0.19 0.50 13.02 0.7222361 44.35 0.5117084 7.41 17.33 0.83 932.64 0.80 899.70 0.57 0.16 0.28 0.28 0.19 1.13 0.10 1.22 3.71 0.19 0.50 13.06 0.7224520 44.62 0.5117013 7.47 17.34 0.83 931.91 0.81 900.45 0.57 0.16 0.29 0.29 0.18 1.13 0.10 1.23 3.68 0.18 0.50 13.10 0.7226611 44.88 0.5116944 7.53 17.34 0.83 931.18 0.81 901.18 0.57 0.17 0.29 0.29 0.18 1.13 0.10 1.23 3.65 0.18 0.50 13.15 0.7228634 45.13 0.5116876 7.59 17.34 0.83 930.45 0.81 901.91 0.57 0.17 0.30 0.30 0.18 1.14 0.10 1.23 3.62 0.18 0.50 13.20 0.7230591 45.38 0.5116810 7.65 17.35 0.83 929.73 0.81 902.63 0.57 0.17 0.31 0.31 0.17 1.14 0.10 1.24 3.59 0.17 0.50 13.25 0.7232482 45.63 0.5116744 7.70 17.35 0.83 929.00 0.81 903.34 0.58 0.18 0.31 0.31 0.17 1.15 0.10 1.24 3.56 0.17 0.50 13.31 0.7234309 45.87 0.5116680 7.76 17.35 0.82 928.27 0.81 904.05 0.58 0.18 0.32 0.32 0.17 1.15 0.10 1.25 3.53 0.17 0.50 13.38 0.7236074 46.11 0.5116616 7.81 17.36 0.82 927.54 0.81 904.75 0.58 0.18 0.32 0.32 0.17 1.15 0.10 1.25 3.50 0.17 0.50 13.44 0.7237777 46.35 0.5116554 7.87 17.36 0.82 926.81 0.81 905.44 0.58 0.19 0.33 0.33 0.16 1.16 0.10 1.25 3.47 0.16 0.50 13.51 0.7239420 46.58 0.5116493 7.92 17.36 0.82 926.08 0.81 906.12 0.58 0.19 0.33 0.33 0.16 1.16 0.10 1.26 3.44 0.16 0.50 13.59 0.7241005 46.80 0.5116433 7.97 17.37 0.82 925.35 0.81 906.80 0.58 0.19 0.34 0.34 0.16 1.17 0.10 1.26 3.41 0.16 0.50 13.67 0.7242533 47.03 0.5116374 8.03 17.37 0.82 924.63 0.81 907.48 0.58 0.19 0.34 0.34 0.16 1.17 0.10 1.27 3.38 0.16 0.50 13.75 0.7244007 47.24 0.5116316 8.08 17.37 0.82 923.90 0.81 908.14 0.59 0.20 0.35 0.35 0.15 1.17 0.10 1.27 3.36 0.15 0.50 13.83 0.7245426 47.46 0.5116259 8.13 17.38 0.82 923.17 0.81 908.80 0.59 0.20 0.35 0.35 0.15 1.18 0.10 1.27 3.33 0.15 0.50 13.92 0.7246794 47.67 0.5116203 8.18 17.38 0.82 922.44 0.81 909.46 0.59 0.20 0.36 0.36 0.15 1.18 0.10 1.28 3.30 0.15 0.50 14.01 0.7248111 47.87 0.5116148 8.22 17.38 0.82 921.71 0.81 910.10 0.59 0.21 0.36 0.36 0.15 1.18 0.10 1.28 3.27 0.15 0.50 14.10 0.7249380 48.08 0.5116094 8.27 17.38 0.82 920.98 0.81 910.75 0.59 0.21 0.37 0.37 0.14 1.19 0.10 1.28 3.25 0.14 0.50 14.19 0.7250602 48.27 0.5116041 8.32 17.39 0.82 920.25 0.81 911.38 0.60 0.21 0.37 0.37 0.14 1.19 0.10 1.29 3.22 0.14 0.50 14.29 0.7251778 48.47 0.5115989 8.36 17.39 0.82 919.53 0.81 912.02 0.60 0.22 0.38 0.38 0.14 1.19 0.10 1.29 3.19 0.14 0.50 14.39 0.7252911 48.66 0.5115938 8.41 17.39 0.82 918.80 0.81 912.64 0.60 0.22 0.39 0.39 0.14 1.20 0.10 1.29 3.17 0.14 0.50 14.50 0.7254001 48.84 0.5115887 8.45 17.40 0.82 918.07 0.81 913.27 0.60 0.22 0.39 0.39 0.14 1.20 0.10 1.30 3.14 0.14 0.50 14.60 0.7255051 49.02 0.5115838 8.49 17.40 0.82 917.34 0.81 913.88 0.60 0.23 0.40 0.40 0.13 1.20 0.10 1.30 3.12 0.13 0.50 14.71 0.7256061 49.20 0.5115789 8.54 17.40 0.82 916.61 0.82 914.49 0.61 0.23 0.40 0.40 0.13 1.21 0.10 1.30 3.09 0.13 0.50 14.82 0.7257033 49.37 0.5115742 8.58 17.40 0.82 915.88 0.82 915.10 0.61 0.23 0.41 0.41 0.13 1.21 0.10 1.31 3.07 0.13 0.50 14.93 0.7257969 49.54 0.5115695 8.62 17.41

147 EC-RAXFC Results - Melts Page MODEL D

Equilibration Parameters tlm 1184 degC 18O/16O in magma 5.8 Magma a 450 Mro 0.5 Element Name Sr Nd Pb Teq Norm 0.833 tmo 1184 degC 18O/16O in assimilant 0.5 Magma b -11 Episodic Recharge Magma: conc. 419 17 2 Teq deg C 940.65428 tla 1129 degC 18O/16O in recharge 5.8 Assimilant a 400 Episode deltaMri Tm,i mr,i d,i bulk Dmo 4 0.6 0.5 Mm 0.865780299 tao 450 degC Oxygen conc magma 0.47 Assimilant b -11 1 0.2 1000 0.3 2 enthalpy 0 0 0 Mao 1.39027155 tlr 1184 degC Oxygen conc assimilant 0.5 Recharge Magma a 450 2 0.2 1175 0.3 2 Assimilant: conc. 255 44.5 8.3 Ma* 0.538687355 tro 1184 degC Oxygen conc recharge 0.47 Recharge Magma b -11 3 0.1 1155 0.3 2 bulk Dao 6 0.7 0.7 Mc 1.076270911 ts 750 degC enthalpy 0 0 0 Men 0.096636145 cpm 1100 J/kg K Recharge: conc. 419 17 2 Ms 1.172907056 cpa 1000 J/kg K bulk Dro 4 0.5 0.5 fa 0.387469164 cpr 1100 J/kg K enthalpy 0 0 0 fm 0.218061963 hm 400000 J/kg Isotope Name 87Sr/86Sr 143Nd/144Nd 206Pb/204Pb fr 0.218061963 ha 350000 J/kg ratio in magma 0.7054 0.512483 16.79 hr 400000 J/kg ratio in assimilant 0.728666 0.51112 17.62 X 1 Normalized fraction of Wallrock melt ratio in recharge 0.7054 0.512483 16.79 mixed into Magma body

Norm T T magma Norm T T assim magma (deg C) assim (deg C) Mm fa Ma* X Ma* fm Mc Men Ms delO18 fr Mr Sr 87Sr/86Sr Nd 143Nd/144Nd Pb 206Pb/204Pb

1.00 1184.00 0.50 450.00 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 419.00 0.705400 17.00 0.512483 2.00 16.79 1.00 1183.27 0.50 450.62 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.82 0.705400 17.00 0.512483 2.00 16.79 1.00 1182.54 0.50 451.24 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.64 0.705400 17.00 0.512483 2.00 16.79 1.00 1181.81 0.50 451.86 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.45 0.705400 17.00 0.512483 2.00 16.79 1.00 1181.09 0.50 452.48 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.26 0.705400 17.00 0.512483 2.00 16.79 1.00 1180.36 0.50 453.11 1.00 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.00 418.06 0.705400 17.01 0.512483 2.00 16.79 1.00 1179.63 0.50 453.75 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 417.85 0.705400 17.01 0.512483 2.00 16.79 1.00 1178.90 0.50 454.40 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 417.62 0.705400 17.01 0.512483 2.00 16.79 1.00 1178.17 0.50 455.05 1.01 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.01 417.39 0.705400 17.01 0.512483 2.00 16.79 1.00 1177.44 0.50 455.73 1.02 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.02 417.14 0.705400 17.01 0.512483 2.00 16.79 1.00 1176.71 0.50 456.42 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.03 416.87 0.705400 17.01 0.512483 2.00 16.79 0.99 1175.99 0.50 457.14 1.03 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.04 416.59 0.705400 17.01 0.512483 2.00 16.79 0.99 1175.26 0.50 457.88 1.04 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.05 416.30 0.705400 17.02 0.512483 2.00 16.79 0.99 1174.53 0.50 458.65 1.05 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.06 415.99 0.705400 17.02 0.512483 2.00 16.79 0.99 1173.80 0.50 459.44 1.07 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.07 415.68 0.705400 17.02 0.512483 2.00 16.79 0.99 1173.07 0.50 460.26 1.08 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.08 415.35 0.705400 17.02 0.512483 2.00 16.79 0.99 1172.34 0.50 461.09 1.09 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.09 415.02 0.705400 17.02 0.512483 2.00 16.79 0.99 1171.61 0.50 461.95 1.10 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.11 414.70 0.705400 17.03 0.512483 2.00 16.79 0.99 1170.89 0.51 462.81 1.12 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.12 414.37 0.705400 17.03 0.512483 2.00 16.79 0.99 1170.16 0.51 463.67 1.13 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.13 414.05 0.705400 17.03 0.512483 2.00 16.79 0.99 1169.43 0.51 464.54 1.14 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.14 413.73 0.705400 17.03 0.512483 2.00 16.79 0.99 1168.70 0.51 465.40 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.15 413.42 0.705400 17.03 0.512483 2.00 16.79 0.99 1167.97 0.51 466.26 1.15 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.16 413.12 0.705400 17.03 0.512483 2.00 16.79 0.99 1167.24 0.51 467.11 1.16 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 412.81 0.705400 17.04 0.512483 2.00 16.79 0.99 1166.51 0.51 467.96 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.17 412.51 0.705400 17.04 0.512483 2.01 16.79 0.99 1165.79 0.51 468.79 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 412.21 0.705400 17.04 0.512483 2.01 16.79 0.99 1165.06 0.51 469.62 1.17 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 411.91 0.705400 17.04 0.512483 2.01 16.79 0.99 1164.33 0.51 470.45 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.18 411.62 0.705400 17.04 0.512483 2.01 16.79 0.99 1163.60 0.51 471.27 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.01 5.80 0.99 0.19 411.32 0.705400 17.04 0.512483 2.01 16.79 0.99 1162.87 0.51 472.08 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 411.02 0.705400 17.05 0.512483 2.01 16.79 0.99 1162.14 0.51 472.90 1.18 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 410.71 0.705400 17.05 0.512483 2.01 16.79 0.98 1161.41 0.51 473.71 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.19 410.40 0.705400 17.05 0.512483 2.01 16.79 0.98 1160.69 0.51 474.53 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 410.09 0.705400 17.05 0.512483 2.01 16.79 0.98 1159.96 0.51 475.35 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 409.77 0.705400 17.05 0.512483 2.01 16.79 0.98 1159.23 0.51 476.18 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 409.45 0.705400 17.06 0.512483 2.01 16.79 0.98 1158.50 0.51 477.02 1.19 0.00 0.00 0.00 0.99 0.01 0.00 0.02 5.80 0.99 0.20 409.12 0.705400 17.06 0.512483 2.01 16.79 0.98 1157.77 0.52 477.88 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 408.78 0.705400 17.06 0.512483 2.01 16.79 0.98 1157.04 0.52 478.76 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 408.43 0.705400 17.06 0.512483 2.01 16.79 0.98 1156.31 0.52 479.66 1.20 0.00 0.00 0.00 0.99 0.02 0.00 0.02 5.80 0.99 0.21 408.07 0.705400 17.06 0.512483 2.01 16.79 0.98 1155.59 0.52 480.59 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 407.70 0.705400 17.07 0.512483 2.01 16.79 0.98 1154.86 0.52 481.54 1.21 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.22 407.32 0.705400 17.07 0.512483 2.01 16.79 0.98 1154.13 0.52 482.52 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.23 406.93 0.705400 17.07 0.512483 2.01 16.79 0.98 1153.40 0.52 483.51 1.22 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 406.54 0.705400 17.07 0.512483 2.01 16.79 0.98 1152.67 0.52 484.52 1.23 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.24 406.14 0.705400 17.07 0.512483 2.01 16.79 0.98 1151.94 0.52 485.54 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.25 405.73 0.705400 17.08 0.512483 2.01 16.79 0.98 1151.21 0.52 486.57 1.24 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 405.32 0.705400 17.08 0.512483 2.01 16.79 0.98 1150.49 0.52 487.59 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.26 404.90 0.705400 17.08 0.512483 2.01 16.79 0.98 1149.76 0.52 488.61 1.25 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 404.48 0.705400 17.08 0.512483 2.01 16.79 0.98 1149.03 0.52 489.62 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.27 404.06 0.705400 17.09 0.512483 2.01 16.79 0.98 1148.30 0.52 490.62 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 403.64 0.705400 17.09 0.512483 2.01 16.79 0.98 1147.57 0.52 491.60 1.26 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 403.21 0.705400 17.09 0.512483 2.01 16.79 0.97 1146.84 0.53 492.58 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.28 402.77 0.705400 17.09 0.512483 2.01 16.79 0.97 1146.11 0.53 493.54 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.02 5.80 0.98 0.29 402.33 0.705400 17.10 0.512483 2.01 16.79 0.97 1145.39 0.53 494.50 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 401.89 0.705400 17.10 0.512483 2.01 16.79 0.97 1144.66 0.53 495.45 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 401.44 0.705400 17.10 0.512483 2.01 16.79 0.97 1143.93 0.53 496.38 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 400.99 0.705400 17.10 0.512483 2.01 16.79 0.97 1143.20 0.53 497.32 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 400.53 0.705400 17.11 0.512483 2.02 16.79 0.97 1142.47 0.53 498.24 1.27 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.29 400.06 0.705400 17.11 0.512483 2.02 16.79 0.97 1141.74 0.53 499.17 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 399.59 0.705400 17.11 0.512483 2.02 16.79 0.97 1141.01 0.53 500.09 1.28 0.00 0.00 0.00 0.98 0.02 0.00 0.03 5.80 0.98 0.30 399.11 0.705400 17.12 0.512483 2.02 16.79 0.97 1140.29 0.53 501.01 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 398.62 0.705400 17.12 0.512483 2.02 16.79 0.97 1139.56 0.53 501.93 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 398.13 0.705400 17.12 0.512483 2.02 16.79 0.97 1138.83 0.53 502.84 1.28 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 397.62 0.705400 17.12 0.512483 2.02 16.79 0.97 1138.10 0.53 503.76 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 397.11 0.705400 17.13 0.512483 2.02 16.79 0.97 1137.37 0.53 504.68 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 396.59 0.705400 17.13 0.512483 2.02 16.79 0.97 1136.64 0.53 505.60 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 396.07 0.705400 17.13 0.512483 2.02 16.79 0.97 1135.91 0.54 506.52 1.27 0.00 0.00 0.00 0.98 0.03 0.00 0.03 5.80 0.98 0.30 395.53 0.705400 17.14 0.512483 2.02 16.79 0.97 1135.19 0.54 507.44 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 394.98 0.705400 17.14 0.512483 2.02 16.79 0.97 1134.46 0.54 508.37 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 394.43 0.705400 17.14 0.512483 2.02 16.79 0.97 1133.73 0.54 509.29 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 393.87 0.705400 17.15 0.512483 2.02 16.79 0.97 1133.00 0.54 510.22 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.03 5.80 0.97 0.30 393.29 0.705400 17.15 0.512483 2.02 16.79 0.96 1132.27 0.54 511.15 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 392.71 0.705400 17.15 0.512483 2.02 16.79 0.96 1131.54 0.54 512.09 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 392.12 0.705400 17.16 0.512483 2.02 16.79 0.96 1130.81 0.54 513.03 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 391.52 0.705400 17.16 0.512483 2.02 16.79 0.96 1130.09 0.54 513.97 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 390.91 0.705400 17.16 0.512483 2.02 16.79 0.96 1129.36 0.54 514.91 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 390.29 0.705400 17.17 0.512483 2.02 16.79 0.96 1128.63 0.54 515.86 1.27 0.00 0.00 0.00 0.97 0.03 0.00 0.04 5.80 0.97 0.30 389.65 0.705400 17.17 0.512483 2.02 16.79 0.96 1127.90 0.54 516.81 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 389.01 0.705400 17.17 0.512483 2.02 16.79 0.96 1127.17 0.54 517.76 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 388.36 0.705400 17.18 0.512483 2.03 16.79 0.96 1126.44 0.54 518.72 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 387.70 0.705400 17.18 0.512483 2.03 16.79 0.96 1125.71 0.54 519.68 1.27 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 387.02 0.705400 17.19 0.512483 2.03 16.79 0.96 1124.99 0.54 520.64 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 386.34 0.705400 17.19 0.512483 2.03 16.79 0.96 1124.26 0.55 521.61 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 385.64 0.705400 17.19 0.512483 2.03 16.79 0.96 1123.53 0.55 522.58 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 384.93 0.705400 17.20 0.512483 2.03 16.79 0.96 1122.80 0.55 523.56 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.04 5.80 0.97 0.30 384.21 0.705400 17.20 0.512483 2.03 16.79 0.96 1122.07 0.55 524.54 1.26 0.00 0.00 0.00 0.97 0.04 0.00 0.05 5.80 0.97 0.30 383.48 0.705400 17.21 0.512483 2.03 16.79 0.96 1121.34 0.55 525.52 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 382.74 0.705400 17.21 0.512483 2.03 16.79 0.96 1120.61 0.55 526.51 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 381.99 0.705400 17.22 0.512483 2.03 16.79

148 0.96 1119.88 0.55 527.50 1.26 0.00 0.00 0.00 0.96 0.04 0.00 0.05 5.80 0.96 0.30 381.22 0.705400 17.22 0.512483 2.03 16.79 0.96 1119.16 0.55 528.49 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 380.44 0.705400 17.23 0.512483 2.03 16.79 0.96 1118.43 0.55 529.49 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 379.65 0.705400 17.23 0.512483 2.03 16.79 0.95 1117.70 0.55 530.50 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 378.85 0.705400 17.24 0.512483 2.03 16.79 0.95 1116.97 0.55 531.50 1.26 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 378.04 0.705400 17.24 0.512483 2.03 16.79 0.95 1116.24 0.55 532.52 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 377.21 0.705400 17.25 0.512483 2.04 16.79 0.95 1115.51 0.55 533.53 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 376.37 0.705400 17.25 0.512483 2.04 16.79 0.95 1114.78 0.55 534.56 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.05 5.80 0.96 0.30 375.51 0.705400 17.26 0.512483 2.04 16.79 0.95 1114.06 0.56 535.58 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 374.65 0.705400 17.26 0.512483 2.04 16.79 0.95 1113.33 0.56 536.61 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 373.76 0.705400 17.27 0.512483 2.04 16.79 0.95 1112.60 0.56 537.65 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 372.87 0.705400 17.27 0.512483 2.04 16.79 0.95 1111.87 0.56 538.69 1.25 0.00 0.00 0.00 0.96 0.05 0.00 0.06 5.80 0.96 0.30 371.96 0.705400 17.28 0.512483 2.04 16.79 0.95 1111.14 0.56 539.74 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 371.04 0.705400 17.28 0.512483 2.04 16.79 0.95 1110.41 0.56 540.79 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 370.10 0.705400 17.29 0.512483 2.04 16.79 0.95 1109.68 0.56 541.84 1.25 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 369.15 0.705400 17.29 0.512483 2.04 16.79 0.95 1108.96 0.56 542.90 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 368.19 0.705400 17.30 0.512483 2.04 16.79 0.95 1108.23 0.56 543.97 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 367.21 0.705400 17.31 0.512483 2.04 16.79 0.95 1107.50 0.56 545.04 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.06 5.80 0.95 0.30 366.22 0.705400 17.31 0.512483 2.05 16.79 0.95 1106.77 0.56 546.12 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 365.21 0.705400 17.32 0.512483 2.05 16.79 0.95 1106.04 0.56 547.20 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 364.18 0.705400 17.33 0.512483 2.05 16.79 0.95 1105.31 0.56 548.29 1.24 0.00 0.00 0.00 0.95 0.06 0.00 0.07 5.80 0.95 0.30 363.14 0.705400 17.33 0.512483 2.05 16.79 0.95 1104.58 0.56 549.38 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 362.09 0.705400 17.34 0.512483 2.05 16.79 0.95 1103.86 0.57 550.48 1.24 0.00 0.00 0.00 0.95 0.07 0.00 0.07 5.80 0.95 0.30 361.02 0.705400 17.35 0.512483 2.05 16.79 0.94 1103.13 0.57 551.59 1.24 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 359.93 0.705400 17.35 0.512483 2.05 16.79 0.94 1102.40 0.57 552.70 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 358.83 0.705400 17.36 0.512483 2.05 16.79 0.94 1101.67 0.57 553.82 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.07 5.80 0.94 0.30 357.72 0.705400 17.37 0.512483 2.05 16.79 0.94 1100.94 0.57 554.94 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 356.58 0.705400 17.38 0.512483 2.05 16.79 0.94 1100.21 0.57 556.07 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 355.44 0.705400 17.38 0.512483 2.06 16.79 0.94 1099.48 0.57 557.21 1.23 0.00 0.00 0.00 0.94 0.07 0.00 0.08 5.80 0.94 0.30 354.27 0.705400 17.39 0.512483 2.06 16.79 0.94 1098.76 0.57 558.35 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 353.09 0.705400 17.40 0.512483 2.06 16.79 0.94 1098.03 0.57 559.50 1.23 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 351.89 0.705400 17.41 0.512483 2.06 16.79 0.94 1097.30 0.57 560.65 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 350.67 0.705400 17.41 0.512483 2.06 16.79 0.94 1096.57 0.57 561.81 1.22 0.00 0.00 0.00 0.94 0.08 0.00 0.08 5.80 0.94 0.30 349.44 0.705400 17.42 0.512483 2.06 16.79 0.94 1095.84 0.57 562.98 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 348.19 0.705400 17.43 0.512483 2.06 16.79 0.94 1095.11 0.57 564.16 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 346.93 0.705400 17.44 0.512483 2.06 16.79 0.94 1094.38 0.58 565.34 1.22 0.00 0.00 0.00 0.93 0.08 0.00 0.09 5.80 0.93 0.30 345.64 0.705400 17.45 0.512483 2.07 16.79 0.94 1093.66 0.58 566.53 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 344.34 0.705400 17.46 0.512483 2.07 16.79 0.94 1092.93 0.58 567.72 1.22 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 343.02 0.705400 17.47 0.512483 2.07 16.79 0.94 1092.20 0.58 568.93 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 341.69 0.705400 17.47 0.512483 2.07 16.79 0.94 1091.47 0.58 570.14 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.09 5.80 0.93 0.30 340.33 0.705400 17.48 0.512483 2.07 16.79 0.94 1090.74 0.58 571.36 1.21 0.00 0.00 0.00 0.93 0.09 0.00 0.10 5.80 0.93 0.30 338.96 0.705400 17.49 0.512483 2.07 16.79 0.94 1090.01 0.58 572.58 1.21 0.00 0.00 0.00 0.92 0.09 0.00 0.10 5.80 0.92 0.30 337.57 0.705400 17.50 0.512483 2.07 16.79 0.94 1089.28 0.58 573.81 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 336.16 0.705400 17.51 0.512483 2.07 16.79 0.93 1088.56 0.58 575.05 1.21 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 334.74 0.705400 17.52 0.512483 2.08 16.79 0.93 1087.83 0.58 576.30 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 333.29 0.705400 17.53 0.512483 2.08 16.79 0.93 1087.10 0.58 577.56 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.10 5.80 0.92 0.30 331.83 0.705400 17.54 0.512483 2.08 16.79 0.93 1086.37 0.58 578.82 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 330.35 0.705400 17.55 0.512483 2.08 16.79 0.93 1085.64 0.59 580.09 1.20 0.00 0.00 0.00 0.92 0.10 0.00 0.11 5.80 0.92 0.30 328.85 0.705400 17.56 0.512483 2.08 16.79 0.93 1084.91 0.59 581.37 1.20 0.00 0.00 0.00 0.92 0.11 0.00 0.11 5.80 0.92 0.30 327.33 0.705400 17.58 0.512483 2.08 16.79 0.93 1084.18 0.59 582.66 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 325.80 0.705400 17.59 0.512483 2.09 16.79 0.93 1083.46 0.59 583.96 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.11 5.80 0.91 0.30 324.24 0.705400 17.60 0.512483 2.09 16.79 0.93 1082.73 0.59 585.26 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 322.67 0.705400 17.61 0.512483 2.09 16.79 0.93 1082.00 0.59 586.57 1.19 0.00 0.00 0.00 0.91 0.11 0.00 0.12 5.80 0.91 0.30 321.07 0.705400 17.62 0.512483 2.09 16.79 0.93 1081.27 0.59 587.90 1.19 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 319.46 0.705400 17.63 0.512483 2.09 16.79 0.93 1080.54 0.59 589.23 1.18 0.00 0.00 0.00 0.91 0.12 0.00 0.12 5.80 0.91 0.30 317.83 0.705400 17.64 0.512483 2.09 16.79 0.93 1079.81 0.59 590.57 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.12 5.80 0.90 0.30 316.18 0.705400 17.66 0.512483 2.10 16.79 0.93 1079.08 0.59 591.91 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 314.51 0.705400 17.67 0.512483 2.10 16.79 0.93 1078.36 0.59 593.27 1.18 0.00 0.00 0.00 0.90 0.12 0.00 0.13 5.80 0.90 0.30 312.82 0.705400 17.68 0.512483 2.10 16.79 0.93 1077.63 0.60 594.64 1.18 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 311.11 0.705400 17.69 0.512483 2.10 16.79 0.93 1076.90 0.60 596.01 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 309.39 0.705400 17.71 0.512483 2.10 16.79 0.93 1076.17 0.60 597.40 1.17 0.00 0.00 0.00 0.90 0.13 0.00 0.13 5.80 0.90 0.30 307.64 0.705400 17.72 0.512483 2.11 16.79 0.93 1075.44 0.60 598.79 1.17 0.00 0.00 0.00 0.89 0.13 0.00 0.14 5.80 0.89 0.30 305.88 0.705400 17.74 0.512483 2.11 16.79 0.93 1074.71 0.60 600.19 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 304.09 0.705400 17.75 0.512483 2.11 16.79 0.92 1073.98 0.60 601.60 1.17 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 302.29 0.705400 17.76 0.512483 2.11 16.79 0.92 1073.26 0.60 603.03 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.14 5.80 0.89 0.30 300.47 0.705400 17.78 0.512483 2.11 16.79 0.92 1072.53 0.60 604.46 1.16 0.00 0.00 0.00 0.89 0.14 0.00 0.15 5.80 0.89 0.30 298.63 0.705400 17.79 0.512483 2.12 16.79 0.92 1071.80 0.60 605.90 1.16 0.00 0.00 0.00 0.89 0.15 0.00 0.15 5.80 0.89 0.30 296.77 0.705400 17.81 0.512483 2.12 16.79 0.92 1071.07 0.60 607.35 1.16 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 294.89 0.705400 17.82 0.512483 2.12 16.79 0.92 1070.34 0.61 608.81 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.15 5.80 0.88 0.30 293.00 0.705400 17.84 0.512483 2.12 16.79 0.92 1069.61 0.61 610.29 1.15 0.00 0.00 0.00 0.88 0.15 0.00 0.16 5.80 0.88 0.30 291.08 0.705400 17.85 0.512483 2.13 16.79 0.92 1068.88 0.61 611.77 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 289.15 0.705400 17.87 0.512483 2.13 16.79 0.92 1068.16 0.61 613.26 1.15 0.00 0.00 0.00 0.88 0.16 0.00 0.16 5.80 0.88 0.30 287.20 0.705400 17.89 0.512483 2.13 16.79 0.92 1067.43 0.61 614.76 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.16 5.80 0.87 0.30 285.23 0.705400 17.90 0.512483 2.13 16.79 0.92 1066.70 0.61 616.28 1.14 0.00 0.00 0.00 0.87 0.16 0.00 0.17 5.80 0.87 0.30 283.24 0.705400 17.92 0.512483 2.14 16.79 0.92 1065.97 0.61 617.80 1.14 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 281.23 0.705400 17.94 0.512483 2.14 16.79 0.92 1065.24 0.61 619.33 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.17 5.80 0.87 0.30 279.21 0.705400 17.95 0.512483 2.14 16.79 0.92 1064.51 0.61 620.88 1.13 0.00 0.00 0.00 0.87 0.17 0.00 0.18 5.80 0.87 0.30 277.16 0.705400 17.97 0.512483 2.14 16.79 0.92 1063.78 0.61 622.43 1.13 0.00 0.00 0.00 0.86 0.17 0.00 0.18 5.80 0.86 0.30 275.10 0.705400 17.99 0.512483 2.15 16.79 0.92 1063.06 0.62 624.00 1.13 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 273.03 0.705400 18.01 0.512483 2.15 16.79 0.92 1062.33 0.62 625.58 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.18 5.80 0.86 0.30 270.93 0.705400 18.03 0.512483 2.15 16.79 0.92 1061.60 0.62 627.17 1.12 0.00 0.00 0.00 0.86 0.18 0.00 0.19 5.80 0.86 0.30 268.82 0.705400 18.05 0.512483 2.15 16.79 0.92 1060.87 0.62 628.76 1.12 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 266.69 0.705400 18.06 0.512483 2.16 16.79 0.92 1060.14 0.62 630.38 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.19 5.80 0.85 0.30 264.55 0.705400 18.08 0.512483 2.16 16.79 0.91 1059.41 0.62 632.00 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 262.39 0.705400 18.10 0.512483 2.16 16.79 0.91 1058.68 0.62 633.63 1.11 0.00 0.00 0.00 0.85 0.19 0.00 0.20 5.80 0.85 0.30 260.21 0.705400 18.12 0.512483 2.17 16.79 0.91 1057.96 0.62 635.27 1.11 0.00 0.00 0.00 0.85 0.20 0.00 0.20 5.80 0.85 0.30 258.02 0.705400 18.15 0.512482 2.17 16.79 0.91 1057.23 0.62 636.93 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.20 5.80 0.84 0.30 255.81 0.705400 18.17 0.512482 2.17 16.79 0.91 1056.50 0.63 638.60 1.10 0.00 0.00 0.00 0.84 0.20 0.00 0.21 5.80 0.84 0.30 253.58 0.705400 18.19 0.512482 2.18 16.79 0.91 1055.77 0.63 640.27 1.10 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 251.34 0.705400 18.21 0.512482 2.18 16.79 0.91 1055.04 0.63 641.96 1.09 0.00 0.00 0.00 0.84 0.21 0.00 0.21 5.80 0.84 0.30 249.09 0.705400 18.23 0.512482 2.18 16.79 0.91 1054.31 0.63 643.67 1.09 0.00 0.00 0.00 0.83 0.21 0.00 0.22 5.80 0.83 0.30 246.82 0.705400 18.25 0.512482 2.19 16.79 0.91 1053.58 0.63 645.38 1.09 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 244.54 0.705401 18.28 0.512482 2.19 16.79 0.91 1052.86 0.63 647.10 1.08 0.00 0.00 0.00 0.83 0.22 0.00 0.22 5.80 0.83 0.30 242.24 0.705401 18.30 0.512482 2.19 16.79 0.91 1052.13 0.63 648.84 1.08 0.00 0.00 0.00 0.82 0.22 0.00 0.23 5.80 0.82 0.30 239.94 0.705401 18.32 0.512482 2.20 16.79 0.91 1051.40 0.63 650.59 1.08 0.00 0.00 0.00 0.82 0.23 0.00 0.23 5.80 0.82 0.30 237.61 0.705401 18.35 0.512482 2.20 16.79 0.91 1050.67 0.64 652.35 1.07 0.00 0.00 0.00 0.82 0.23 0.00 0.24 5.80 0.82 0.30 235.28 0.705401 18.37 0.512482 2.20 16.79 0.91 1049.94 0.64 654.12 1.07 0.00 0.00 0.00 0.82 0.24 0.00 0.24 5.80 0.82 0.30 232.93 0.705401 18.40 0.512482 2.21 16.79 0.91 1049.21 0.64 655.90 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.24 5.80 0.81 0.30 230.57 0.705401 18.42 0.512482 2.21 16.79 0.91 1048.48 0.64 657.70 1.06 0.00 0.00 0.00 0.81 0.24 0.00 0.25 5.80 0.81 0.30 228.21 0.705401 18.45 0.512482 2.22 16.79 0.91 1047.76 0.64 659.50 1.06 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 225.82 0.705401 18.48 0.512482 2.22 16.79 0.91 1047.03 0.64 661.32 1.05 0.00 0.00 0.00 0.81 0.25 0.00 0.25 5.80 0.81 0.30 223.43 0.705401 18.50 0.512482 2.22 16.79 0.91 1046.30 0.64 663.15 1.05 0.00 0.00 0.00 0.80 0.25 0.00 0.26 5.80 0.80 0.30 221.03 0.705401 18.53 0.512482 2.23 16.79 0.91 1045.57 0.64 665.00 1.05 0.00 0.00 0.00 0.80 0.26 0.00 0.26 5.80 0.80 0.30 218.62 0.705401 18.56 0.512482 2.23 16.79 0.90 1044.84 0.65 666.85 1.04 0.00 0.00 0.00 0.80 0.26 0.00 0.27 5.80 0.80 0.30 216.20 0.705401 18.59 0.512482 2.24 16.79 0.90 1044.11 0.65 668.72 1.04 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 213.78 0.705401 18.61 0.512482 2.24 16.79 0.90 1043.38 0.65 670.59 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.27 5.80 0.79 0.30 211.34 0.705401 18.64 0.512481 2.24 16.79 0.90 1042.66 0.65 672.48 1.03 0.00 0.00 0.00 0.79 0.27 0.00 0.28 5.80 0.79 0.30 208.90 0.705401 18.67 0.512481 2.25 16.79 0.90 1041.93 0.65 674.38 1.03 0.00 0.00 0.00 0.78 0.28 0.00 0.28 5.80 0.78 0.30 206.45 0.705401 18.70 0.512481 2.25 16.79 0.90 1041.20 0.65 676.30 1.02 0.00 0.00 0.00 0.78 0.28 0.00 0.29 5.80 0.78 0.30 203.99 0.705402 18.73 0.512481 2.26 16.79 0.90 1040.47 0.65 678.22 1.02 0.00 0.00 0.00 0.78 0.29 0.00 0.29 5.80 0.78 0.30 201.53 0.705402 18.77 0.512481 2.26 16.79 0.90 1039.74 0.65 680.16 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.29 5.80 0.77 0.30 199.06 0.705402 18.80 0.512481 2.27 16.79 0.90 1039.01 0.66 682.10 1.01 0.00 0.00 0.00 0.77 0.29 0.00 0.30 5.80 0.77 0.30 196.59 0.705402 18.83 0.512481 2.27 16.79 0.90 1038.28 0.66 684.06 1.01 0.00 0.00 0.00 0.77 0.30 0.00 0.30 5.80 0.77 0.30 194.11 0.705402 18.86 0.512481 2.28 16.79 0.90 1037.56 0.66 686.03 1.00 0.00 0.00 0.00 0.76 0.30 0.00 0.31 5.80 0.76 0.30 191.63 0.705402 18.90 0.512481 2.28 16.79 0.90 1036.83 0.66 688.02 1.00 0.00 0.00 0.00 0.76 0.31 0.00 0.31 5.80 0.76 0.30 189.15 0.705402 18.93 0.512480 2.29 16.79 0.90 1036.10 0.66 690.01 0.99 0.00 0.00 0.00 0.76 0.31 0.00 0.32 5.80 0.76 0.30 186.66 0.705403 18.97 0.512480 2.29 16.79 0.90 1035.37 0.66 692.01 0.99 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 184.18 0.705403 19.00 0.512480 2.30 16.79 0.90 1034.64 0.66 694.03 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.32 5.80 0.75 0.30 181.69 0.705403 19.04 0.512480 2.31 16.79 0.90 1033.91 0.67 696.05 0.98 0.00 0.00 0.00 0.75 0.32 0.00 0.33 5.80 0.75 0.30 179.20 0.705403 19.07 0.512480 2.31 16.79 0.90 1033.18 0.67 698.09 0.98 0.00 0.00 0.00 0.74 0.33 0.00 0.33 5.80 0.74 0.30 176.71 0.705403 19.11 0.512480 2.32 16.79 0.90 1032.46 0.67 700.14 0.97 0.00 0.00 0.00 0.74 0.33 0.00 0.34 5.80 0.74 0.30 174.22 0.705404 19.15 0.512479 2.32 16.79 0.90 1031.73 0.67 702.19 0.97 0.00 0.00 0.00 0.74 0.34 0.00 0.34 5.80 0.74 0.30 171.73 0.705404 19.19 0.512479 2.33 16.79

149 0.90 1031.00 0.67 704.26 0.96 0.00 0.00 0.00 0.73 0.34 0.00 0.35 5.79 0.73 0.30 169.25 0.705404 19.23 0.512479 2.33 16.79 0.89 1030.27 0.67 706.34 0.96 0.00 0.00 0.00 0.73 0.35 0.00 0.35 5.79 0.73 0.30 166.77 0.705405 19.27 0.512479 2.34 16.79 0.89 1029.54 0.67 708.43 0.95 0.00 0.00 0.00 0.73 0.35 0.00 0.36 5.79 0.73 0.30 164.29 0.705405 19.31 0.512478 2.35 16.79 0.89 1028.81 0.68 710.52 0.95 0.00 0.00 0.00 0.72 0.36 0.00 0.36 5.79 0.72 0.30 161.81 0.705405 19.35 0.512478 2.35 16.79 0.89 1028.08 0.68 712.63 0.94 0.00 0.00 0.00 0.72 0.36 0.00 0.37 5.79 0.72 0.30 159.34 0.705406 19.40 0.512478 2.36 16.80 0.89 1027.36 0.68 714.75 0.94 0.00 0.00 0.00 0.72 0.37 0.00 0.37 5.79 0.72 0.30 156.88 0.705406 19.44 0.512477 2.37 16.80 0.89 1026.63 0.68 716.87 0.93 0.00 0.00 0.00 0.71 0.37 0.00 0.38 5.79 0.71 0.30 154.42 0.705407 19.48 0.512477 2.37 16.80 0.89 1025.90 0.68 719.01 0.93 0.00 0.00 0.00 0.71 0.38 0.00 0.38 5.79 0.71 0.30 151.97 0.705408 19.53 0.512477 2.38 16.80 0.89 1025.17 0.68 721.15 0.92 0.00 0.00 0.00 0.70 0.38 0.00 0.39 5.79 0.70 0.30 149.52 0.705408 19.58 0.512476 2.39 16.80 0.89 1024.44 0.68 723.30 0.92 0.00 0.00 0.00 0.70 0.39 0.00 0.39 5.79 0.70 0.30 147.09 0.705409 19.62 0.512476 2.40 16.80 0.89 1023.71 0.69 725.46 0.91 0.00 0.00 0.00 0.70 0.39 0.00 0.40 5.79 0.70 0.30 144.66 0.705410 19.67 0.512475 2.40 16.80 0.89 1022.98 0.69 727.63 0.91 0.00 0.00 0.00 0.69 0.40 0.00 0.40 5.79 0.69 0.30 142.24 0.705411 19.72 0.512475 2.41 16.80 0.89 1022.26 0.69 729.80 0.90 0.00 0.00 0.00 0.69 0.40 0.00 0.41 5.79 0.69 0.30 139.83 0.705411 19.77 0.512474 2.42 16.80 0.89 1021.53 0.69 731.98 0.90 0.00 0.00 0.00 0.68 0.41 0.00 0.41 5.79 0.68 0.30 137.43 0.705412 19.82 0.512473 2.43 16.80 0.89 1020.80 0.69 734.17 0.89 0.00 0.00 0.00 0.68 0.41 0.00 0.42 5.79 0.68 0.30 135.04 0.705414 19.88 0.512473 2.44 16.80 0.89 1020.07 0.69 736.37 0.89 0.00 0.00 0.00 0.68 0.42 0.00 0.42 5.79 0.68 0.30 132.67 0.705415 19.93 0.512472 2.45 16.80 0.89 1019.34 0.69 738.57 0.88 0.00 0.00 0.00 0.67 0.42 0.00 0.43 5.79 0.67 0.30 130.31 0.705416 19.98 0.512471 2.45 16.80 0.89 1018.61 0.70 740.77 0.88 0.00 0.00 0.00 0.67 0.43 0.00 0.43 5.78 0.67 0.30 127.96 0.705417 20.04 0.512471 2.46 16.80 0.89 1017.88 0.70 742.98 0.87 0.00 0.00 0.00 0.66 0.43 0.00 0.44 5.78 0.66 0.30 125.62 0.705419 20.10 0.512470 2.47 16.80 0.89 1017.16 0.70 745.20 0.87 0.00 0.00 0.00 0.66 0.44 0.00 0.44 5.78 0.66 0.30 123.30 0.705421 20.16 0.512469 2.48 16.80 0.89 1016.43 0.70 747.42 0.86 0.00 0.00 0.00 0.66 0.44 0.00 0.45 5.78 0.66 0.30 120.99 0.705423 20.22 0.512468 2.49 16.80 0.88 1015.70 0.70 749.65 0.86 0.00 0.00 0.00 0.65 0.45 0.00 0.45 5.78 0.65 0.30 118.70 0.705425 20.28 0.512467 2.50 16.81 0.88 1014.97 0.70 751.88 0.85 0.00 0.00 0.00 0.65 0.46 0.00 0.46 5.78 0.65 0.30 116.43 0.705427 20.34 0.512466 2.51 16.81 0.88 1014.24 0.70 754.11 0.85 0.00 0.00 0.00 0.64 0.46 0.00 0.46 5.78 0.64 0.30 114.17 0.705429 20.41 0.512464 2.52 16.81 0.88 1013.51 0.71 756.35 0.84 0.00 0.00 0.00 0.64 0.47 0.00 0.47 5.77 0.64 0.30 111.93 0.705432 20.48 0.512463 2.54 16.81 0.88 1012.78 0.71 758.59 0.84 0.00 0.00 0.00 0.63 0.47 0.00 0.48 5.77 0.63 0.30 109.71 0.705435 20.54 0.512462 2.55 16.81 0.88 1012.06 0.71 760.83 0.83 0.00 0.00 0.00 0.63 0.48 0.00 0.48 5.77 0.63 0.30 107.50 0.705438 20.61 0.512460 2.56 16.81 0.88 1011.33 0.71 763.09 0.83 0.00 0.01 0.01 0.63 0.48 0.00 0.49 5.77 0.63 0.30 105.32 0.705442 20.69 0.512459 2.57 16.81 0.88 1010.60 0.71 765.35 0.82 0.00 0.01 0.01 0.62 0.49 0.00 0.49 5.77 0.62 0.30 103.15 0.705446 20.76 0.512457 2.58 16.81 0.88 1009.87 0.71 767.62 0.82 0.00 0.01 0.01 0.62 0.49 0.00 0.50 5.76 0.62 0.30 101.01 0.705450 20.84 0.512455 2.60 16.82 0.88 1009.14 0.72 769.91 0.81 0.00 0.01 0.01 0.61 0.50 0.00 0.50 5.76 0.61 0.30 98.88 0.705455 20.92 0.512453 2.61 16.82 0.88 1008.41 0.72 772.23 0.81 0.00 0.01 0.01 0.61 0.51 0.00 0.51 5.76 0.61 0.30 96.78 0.705460 21.00 0.512451 2.62 16.82 0.88 1007.68 0.72 774.58 0.80 0.01 0.01 0.01 0.60 0.51 0.00 0.52 5.75 0.60 0.30 94.69 0.705466 21.08 0.512449 2.64 16.82 0.88 1006.96 0.72 777.00 0.80 0.01 0.01 0.01 0.60 0.52 0.00 0.52 5.75 0.60 0.30 92.63 0.705473 21.17 0.512446 2.65 16.82 0.88 1006.23 0.72 779.49 0.79 0.01 0.01 0.01 0.60 0.52 0.01 0.53 5.75 0.60 0.30 90.59 0.705481 21.27 0.512443 2.67 16.83 0.88 1005.50 0.72 782.09 0.79 0.01 0.01 0.01 0.59 0.53 0.01 0.54 5.74 0.59 0.30 88.57 0.705489 21.36 0.512440 2.69 16.83 0.88 1004.77 0.73 784.83 0.78 0.01 0.01 0.01 0.59 0.54 0.01 0.54 5.74 0.59 0.31 86.57 0.705500 21.47 0.512437 2.71 16.83 0.88 1004.04 0.73 787.76 0.78 0.01 0.01 0.01 0.58 0.54 0.01 0.55 5.73 0.58 0.31 84.59 0.705512 21.58 0.512433 2.73 16.84 0.88 1003.31 0.73 790.92 0.78 0.01 0.01 0.01 0.58 0.55 0.01 0.56 5.73 0.58 0.31 82.63 0.705526 21.70 0.512428 2.75 16.84 0.88 1002.58 0.73 794.36 0.78 0.01 0.01 0.01 0.57 0.55 0.01 0.57 5.72 0.57 0.32 80.69 0.705544 21.83 0.512423 2.77 16.84 0.88 1001.86 0.74 798.10 0.77 0.01 0.01 0.01 0.57 0.56 0.02 0.58 5.71 0.57 0.33 78.77 0.705566 21.98 0.512416 2.80 16.85 0.87 1001.13 0.74 802.16 0.77 0.01 0.02 0.02 0.56 0.56 0.02 0.59 5.70 0.56 0.33 76.86 0.705593 22.14 0.512408 2.83 16.86 0.87 1000.40 0.74 806.51 0.78 0.01 0.02 0.02 0.56 0.57 0.02 0.60 5.68 0.56 0.34 74.97 0.705627 22.32 0.512399 2.86 16.86 0.87 999.67 0.74 811.13 0.78 0.01 0.02 0.02 0.55 0.58 0.03 0.61 5.66 0.55 0.35 73.10 0.705668 22.53 0.512388 2.90 16.87 0.87 998.94 0.75 815.92 0.78 0.02 0.02 0.02 0.55 0.58 0.04 0.62 5.65 0.55 0.37 71.25 0.705718 22.76 0.512376 2.94 16.88 0.87 998.21 0.75 820.79 0.79 0.02 0.03 0.03 0.55 0.59 0.04 0.63 5.62 0.55 0.38 69.43 0.705777 23.01 0.512362 2.99 16.90 0.87 997.48 0.75 825.65 0.79 0.02 0.03 0.03 0.54 0.60 0.05 0.64 5.60 0.54 0.39 67.64 0.705845 23.28 0.512346 3.05 16.91 0.87 996.75 0.76 830.39 0.80 0.03 0.03 0.03 0.54 0.60 0.05 0.66 5.57 0.54 0.40 65.88 0.705923 23.57 0.512329 3.10 16.92 0.87 996.03 0.76 834.93 0.80 0.03 0.04 0.04 0.53 0.61 0.06 0.67 5.54 0.53 0.42 64.15 0.706009 23.88 0.512311 3.16 16.94 0.87 995.30 0.76 839.21 0.81 0.03 0.04 0.04 0.53 0.62 0.06 0.68 5.51 0.53 0.43 62.47 0.706103 24.20 0.512293 3.23 16.95 0.87 994.57 0.77 843.20 0.81 0.04 0.05 0.05 0.52 0.62 0.07 0.69 5.47 0.52 0.44 60.83 0.706203 24.52 0.512275 3.29 16.97 0.87 993.84 0.77 846.89 0.81 0.04 0.06 0.06 0.52 0.63 0.07 0.70 5.44 0.52 0.45 59.24 0.706308 24.85 0.512257 3.36 16.98 0.87 993.11 0.77 850.28 0.82 0.04 0.06 0.06 0.51 0.64 0.08 0.71 5.41 0.51 0.46 57.69 0.706416 25.18 0.512239 3.42 17.00 0.87 992.38 0.77 853.39 0.82 0.05 0.07 0.07 0.51 0.64 0.08 0.72 5.37 0.51 0.46 56.20 0.706527 25.50 0.512222 3.49 17.01 0.87 991.65 0.78 856.26 0.82 0.05 0.07 0.07 0.50 0.65 0.08 0.73 5.34 0.50 0.47 54.74 0.706641 25.83 0.512205 3.56 17.02 0.87 990.93 0.78 858.90 0.82 0.06 0.08 0.08 0.50 0.66 0.09 0.74 5.31 0.50 0.48 53.33 0.706756 26.14 0.512189 3.62 17.03 0.87 990.20 0.78 861.34 0.82 0.06 0.08 0.08 0.49 0.66 0.09 0.75 5.28 0.49 0.48 51.97 0.706873 26.46 0.512173 3.69 17.04 0.87 989.47 0.78 863.61 0.82 0.06 0.09 0.09 0.49 0.67 0.09 0.76 5.25 0.49 0.48 50.64 0.706992 26.77 0.512158 3.75 17.06 0.87 988.74 0.78 865.74 0.82 0.07 0.09 0.09 0.49 0.68 0.09 0.77 5.22 0.49 0.49 49.36 0.707112 27.07 0.512144 3.81 17.07 0.87 988.01 0.78 867.74 0.82 0.07 0.10 0.10 0.48 0.68 0.09 0.77 5.18 0.48 0.49 48.11 0.707235 27.38 0.512130 3.88 17.08 0.87 987.28 0.78 869.63 0.82 0.07 0.10 0.10 0.48 0.69 0.09 0.78 5.15 0.48 0.49 46.91 0.707361 27.68 0.512116 3.94 17.09 0.86 986.55 0.79 871.44 0.82 0.08 0.11 0.11 0.47 0.70 0.09 0.79 5.12 0.47 0.49 45.74 0.707490 27.98 0.512103 4.00 17.10 0.86 985.83 0.79 873.17 0.82 0.08 0.11 0.11 0.47 0.70 0.09 0.80 5.09 0.47 0.49 44.60 0.707621 28.28 0.512089 4.06 17.10 0.86 985.10 0.79 874.83 0.82 0.09 0.12 0.12 0.46 0.71 0.09 0.81 5.06 0.46 0.49 43.50 0.707757 28.58 0.512077 4.13 17.11 0.86 984.37 0.79 876.44 0.82 0.09 0.12 0.12 0.46 0.72 0.09 0.81 5.03 0.46 0.50 42.44 0.707897 28.88 0.512064 4.19 17.12 0.86 983.64 0.79 877.99 0.82 0.09 0.13 0.13 0.45 0.72 0.10 0.82 5.00 0.45 0.50 41.41 0.708041 29.18 0.512052 4.25 17.13 0.86 982.91 0.79 879.50 0.81 0.10 0.13 0.13 0.45 0.73 0.10 0.83 4.97 0.45 0.50 40.41 0.708189 29.48 0.512039 4.32 17.14 0.86 982.18 0.79 880.98 0.81 0.10 0.14 0.14 0.44 0.74 0.10 0.83 4.94 0.44 0.50 39.45 0.708342 29.78 0.512027 4.38 17.15 0.86 981.45 0.79 882.41 0.81 0.10 0.15 0.15 0.44 0.75 0.10 0.84 4.91 0.44 0.50 38.51 0.708501 30.08 0.512015 4.44 17.15 0.86 980.73 0.79 883.82 0.81 0.11 0.15 0.15 0.44 0.75 0.10 0.85 4.88 0.44 0.50 37.61 0.708664 30.39 0.512003 4.51 17.16 0.86 980.00 0.79 885.20 0.81 0.11 0.16 0.16 0.43 0.76 0.10 0.85 4.85 0.43 0.50 36.74 0.708833 30.69 0.511992 4.57 17.17 0.86 979.27 0.80 886.55 0.81 0.12 0.16 0.16 0.43 0.77 0.10 0.86 4.82 0.43 0.50 35.90 0.709007 30.99 0.511980 4.64 17.18 0.86 978.54 0.80 887.88 0.81 0.12 0.17 0.17 0.42 0.77 0.10 0.87 4.79 0.42 0.50 35.09 0.709187 31.30 0.511969 4.70 17.18 0.86 977.81 0.80 889.18 0.81 0.12 0.17 0.17 0.42 0.78 0.10 0.88 4.75 0.42 0.50 34.31 0.709373 31.60 0.511958 4.77 17.19 0.86 977.08 0.80 890.46 0.80 0.13 0.18 0.18 0.41 0.79 0.10 0.88 4.72 0.41 0.50 33.55 0.709564 31.91 0.511946 4.83 17.20 0.86 976.35 0.80 891.73 0.80 0.13 0.18 0.18 0.41 0.79 0.10 0.89 4.69 0.41 0.50 32.83 0.709761 32.22 0.511935 4.90 17.21 0.86 975.63 0.80 892.97 0.80 0.14 0.19 0.19 0.40 0.80 0.10 0.90 4.66 0.40 0.50 32.13 0.709963 32.53 0.511925 4.96 17.21 0.86 974.90 0.80 894.20 0.80 0.14 0.20 0.20 0.40 0.81 0.10 0.90 4.63 0.40 0.50 31.46 0.710171 32.83 0.511914 5.03 17.22 0.86 974.17 0.80 895.41 0.80 0.15 0.20 0.20 0.39 0.81 0.10 0.91 4.59 0.39 0.50 30.82 0.710384 33.14 0.511903 5.09 17.23 0.86 973.44 0.80 896.60 0.80 0.15 0.21 0.21 0.39 0.82 0.10 0.92 4.56 0.39 0.50 30.20 0.710603 33.45 0.511893 5.16 17.23 0.86 972.71 0.80 897.78 0.80 0.15 0.21 0.21 0.39 0.83 0.10 0.92 4.53 0.39 0.50 29.61 0.710827 33.75 0.511882 5.23 17.24 0.85 971.98 0.80 898.95 0.80 0.16 0.22 0.22 0.38 0.83 0.10 0.93 4.49 0.38 0.50 29.04 0.711056 34.06 0.511872 5.29 17.24 0.85 971.25 0.81 900.09 0.80 0.16 0.23 0.23 0.38 0.84 0.10 0.94 4.46 0.38 0.50 28.50 0.711290 34.36 0.511862 5.36 17.25 0.85 970.53 0.81 901.23 0.80 0.17 0.23 0.23 0.37 0.85 0.10 0.94 4.43 0.37 0.50 27.98 0.711528 34.67 0.511852 5.42 17.26 0.85 969.80 0.81 902.35 0.80 0.17 0.24 0.24 0.37 0.85 0.10 0.95 4.39 0.37 0.50 27.48 0.711771 34.97 0.511842 5.49 17.26 0.85 969.07 0.81 903.46 0.80 0.18 0.25 0.25 0.36 0.86 0.10 0.95 4.36 0.36 0.50 27.01 0.712018 35.27 0.511833 5.56 17.27 0.85 968.34 0.81 904.55 0.80 0.18 0.25 0.25 0.36 0.86 0.10 0.96 4.33 0.36 0.50 26.55 0.712270 35.57 0.511823 5.62 17.27 0.85 967.61 0.81 905.63 0.80 0.19 0.26 0.26 0.36 0.87 0.10 0.97 4.29 0.36 0.50 26.12 0.712525 35.87 0.511814 5.69 17.28 0.85 966.88 0.81 906.70 0.80 0.19 0.27 0.27 0.35 0.88 0.10 0.97 4.26 0.35 0.50 25.71 0.712783 36.17 0.511805 5.75 17.28 0.85 966.15 0.81 907.76 0.80 0.20 0.27 0.27 0.35 0.88 0.10 0.98 4.23 0.35 0.50 25.32 0.713044 36.46 0.511796 5.82 17.29 0.85 965.43 0.81 908.81 0.80 0.20 0.28 0.28 0.34 0.89 0.10 0.99 4.20 0.34 0.50 24.95 0.713309 36.75 0.511787 5.88 17.29 0.85 964.70 0.81 909.85 0.80 0.21 0.29 0.29 0.34 0.90 0.10 0.99 4.16 0.34 0.50 24.60 0.713576 37.04 0.511778 5.94 17.30 0.85 963.97 0.81 910.88 0.80 0.21 0.29 0.29 0.33 0.90 0.10 1.00 4.13 0.33 0.50 24.26 0.713844 37.33 0.511769 6.01 17.30 0.85 963.24 0.81 911.89 0.80 0.22 0.30 0.30 0.33 0.91 0.10 1.00 4.10 0.33 0.50 23.95 0.714115 37.62 0.511761 6.07 17.31 0.85 962.51 0.81 912.90 0.80 0.22 0.31 0.31 0.33 0.91 0.10 1.01 4.06 0.33 0.50 23.65 0.714387 37.90 0.511753 6.13 17.31 0.85 961.78 0.81 913.90 0.80 0.23 0.31 0.31 0.32 0.92 0.10 1.02 4.03 0.32 0.50 23.37 0.714661 38.18 0.511744 6.19 17.32 0.85 961.05 0.82 914.88 0.81 0.23 0.32 0.32 0.32 0.93 0.10 1.02 4.00 0.32 0.50 23.10 0.714935 38.46 0.511736 6.26 17.32 0.85 960.33 0.82 915.86 0.81 0.24 0.33 0.33 0.31 0.93 0.10 1.03 3.97 0.31 0.50 22.85 0.715210 38.73 0.511729 6.32 17.33 0.85 959.60 0.82 916.83 0.81 0.24 0.33 0.33 0.31 0.94 0.10 1.03 3.93 0.31 0.50 22.62 0.715484 39.00 0.511721 6.38 17.33 0.85 958.87 0.82 917.79 0.81 0.25 0.34 0.34 0.31 0.94 0.10 1.04 3.90 0.31 0.50 22.40 0.715759 39.27 0.511713 6.44 17.34 0.85 958.14 0.82 918.75 0.81 0.25 0.35 0.35 0.30 0.95 0.10 1.05 3.87 0.30 0.50 22.19 0.716033 39.53 0.511706 6.50 17.34 0.84 957.41 0.82 919.69 0.81 0.26 0.36 0.36 0.30 0.96 0.10 1.05 3.84 0.30 0.50 22.00 0.716306 39.79 0.511698 6.56 17.34 0.84 956.68 0.82 920.63 0.81 0.26 0.36 0.36 0.30 0.96 0.10 1.06 3.81 0.30 0.50 21.83 0.716577 40.05 0.511691 6.61 17.35 0.84 955.95 0.82 921.56 0.81 0.27 0.37 0.37 0.29 0.97 0.10 1.06 3.77 0.29 0.50 21.67 0.716848 40.30 0.511684 6.67 17.35 0.84 955.23 0.82 922.49 0.82 0.27 0.38 0.38 0.29 0.97 0.10 1.07 3.74 0.29 0.50 21.52 0.717116 40.55 0.511677 6.73 17.35 0.84 954.50 0.82 923.40 0.82 0.28 0.39 0.39 0.28 0.98 0.10 1.08 3.71 0.28 0.50 21.38 0.717383 40.79 0.511670 6.78 17.36 0.84 953.77 0.82 924.31 0.82 0.28 0.39 0.39 0.28 0.98 0.10 1.08 3.68 0.28 0.50 21.25 0.717647 41.04 0.511664 6.84 17.36 0.84 953.04 0.82 925.22 0.82 0.29 0.40 0.40 0.28 0.99 0.10 1.09 3.65 0.28 0.50 21.14 0.717908 41.27 0.511657 6.89 17.37 0.84 952.31 0.82 926.11 0.82 0.29 0.41 0.41 0.27 1.00 0.10 1.09 3.62 0.27 0.50 21.04 0.718167 41.51 0.511651 6.94 17.37 0.84 951.58 0.82 927.01 0.83 0.30 0.42 0.42 0.27 1.00 0.10 1.10 3.59 0.27 0.50 20.95 0.718423 41.74 0.511644 7.00 17.37 0.84 950.85 0.82 927.89 0.83 0.30 0.42 0.42 0.27 1.01 0.10 1.10 3.56 0.27 0.50 20.87 0.718675 41.96 0.511638 7.05 17.38 0.84 950.13 0.82 928.77 0.83 0.31 0.43 0.43 0.26 1.01 0.10 1.11 3.53 0.26 0.50 20.80 0.718924 42.18 0.511632 7.10 17.38 0.84 949.40 0.83 929.65 0.83 0.31 0.44 0.44 0.26 1.02 0.10 1.11 3.50 0.26 0.50 20.74 0.719170 42.40 0.511626 7.15 17.38 0.84 948.67 0.83 930.52 0.83 0.32 0.45 0.45 0.25 1.02 0.10 1.12 3.47 0.25 0.50 20.69 0.719411 42.61 0.511620 7.20 17.38 0.84 947.94 0.83 931.39 0.84 0.33 0.45 0.45 0.25 1.03 0.10 1.12 3.44 0.25 0.50 20.65 0.719649 42.82 0.511615 7.25 17.39 0.84 947.21 0.83 932.25 0.84 0.33 0.46 0.46 0.25 1.03 0.10 1.13 3.42 0.25 0.50 20.62 0.719882 43.02 0.511609 7.29 17.39 0.84 946.48 0.83 933.10 0.84 0.34 0.47 0.47 0.24 1.04 0.10 1.13 3.39 0.24 0.50 20.60 0.720112 43.22 0.511604 7.34 17.39 0.84 945.75 0.83 933.96 0.84 0.34 0.48 0.48 0.24 1.04 0.10 1.14 3.36 0.24 0.50 20.59 0.720337 43.42 0.511598 7.39 17.40 0.84 945.03 0.83 934.80 0.85 0.35 0.48 0.48 0.24 1.05 0.10 1.14 3.33 0.24 0.50 20.59 0.720558 43.61 0.511593 7.43 17.40 0.84 944.30 0.83 935.65 0.85 0.35 0.49 0.49 0.23 1.05 0.10 1.15 3.30 0.23 0.50 20.59 0.720774 43.79 0.511588 7.47 17.40 0.84 943.57 0.83 936.49 0.85 0.36 0.50 0.50 0.23 1.06 0.10 1.15 3.28 0.23 0.50 20.61 0.720986 43.98 0.511583 7.52 17.40 0.83 942.84 0.83 937.33 0.86 0.36 0.51 0.51 0.23 1.06 0.10 1.16 3.25 0.23 0.50 20.63 0.721194 44.15 0.511578 7.56 17.41 0.83 942.11 0.83 938.16 0.86 0.37 0.52 0.52 0.22 1.07 0.10 1.16 3.22 0.22 0.50 20.66 0.721397 44.33 0.511573 7.60 17.41 0.83 941.38 0.83 938.99 0.86 0.38 0.52 0.52 0.22 1.07 0.10 1.17 3.20 0.22 0.50 20.70 0.721595 44.49 0.511568 7.64 17.41 0.83 940.65 0.83 939.82 0.87 0.38 0.53 0.53 0.22 1.08 0.10 1.17 3.17 0.22 0.50 20.74 0.721789 44.66 0.511563 7.68 17.41

150

APPENDIX C

RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF FELDSPAR FROM THE MINGLED MAGMAS

Unit Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B mineral p p p c/i/r r r r Line Numbers Un 5 G 138 139 140 7/13/2009 7/13/2009 7/13/2009 CaO 13.18 12.88 13.57 K2O 0.14 0.15 0.13 SiO2 50.85 51.13 49.93 Al2O3 30.13 30.17 31.25 FeO 0.54 0.51 0.55 Na2O 4.50 4.62 3.99 BaO 0.01 0.00 0.09 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 99.3 99.5 99.5 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

152 Unit Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B mineral pp p c/i/r rr Line Numbers 141 142 Un 6 G 143 7/13/2009 7/13/2009 7/13/2009 CaO 13.43 13.57 13.56 K2O 0.16 0.09 0.13 SiO2 49.88 50.41 50.21 Al2O3 30.98 31.06 30.77 FeO 0.45 0.54 0.53 Na2O 4.11 4.10 4.07 BaO 0.00 0.00 0.04 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 99.0 99.8 99.3 ppm Ti 450.66 431.30 ppm Rb 0.82 0.41 ppm Sr 462.79 511.22 ppm Y 0.31 0.18 ppm Cs 0.11 0.02 ppm Ba 68.73 65.14 ppm La 0.67 0.66 ppm Ce 1.31 1.25 ppm Pr 0.12 0.11 ppm Nd 0.47 0.42 ppm Sm 0.10 0.09 ppm Eu 0.26 0.28 ppm Gd 0.11 0.04 ppm Tb 0.01 0.01 ppm Pb 1.83 1.18

153 Unit Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B mineral pp p c/i/r Line Numbers 146 147 Un 7 G 148 7/13/2009 7/13/2009 7/13/2009 CaO 12.73 13.41 13.98 K2O 0.19 0.13 0.13 SiO2 51.62 50.71 50.13 Al2O3 30.27 30.40 31.15 FeO 0.62 0.52 0.48 Na2O 4.69 4.43 4.08 BaO 0.00 0.02 -0.03 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 100.1 99.6 99.9 ppm Ti 435.29 432.72 ppm Rb 0.29 0.48 ppm Sr 552.86 542.12 ppm Y 0.21 0.25 ppm Cs 0.01 0.02 ppm Ba 59.78 59.16 ppm La 0.64 0.66 ppm Ce 1.19 1.24 ppm Pr 0.12 0.13 ppm Nd 0.44 0.49 ppm Sm 0.04 0.13 ppm Eu 0.30 0.29 ppm Gd 0.04 0.10 ppm Tb 0.00 0.01 ppm Pb 0.86 1.35

154 Unit Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B mineral ppp c/i/r Line Numbers 149 150 151 Un 8 G 7/13/2009 7/13/2009 7/13/2009 CaO 12.63 13.82 12.70 K2O 0.18 0.17 0.19 SiO2 50.89 49.81 51.17 Al2O3 30.46 31.23 30.16 FeO 0.47 0.47 0.46 Na2O 4.70 3.99 4.64 BaO 0.02 0.01 0.07 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 99.3 99.5 99.4 ppm Ti 356.45 381.93 ppm Rb 0.38 0.42 ppm Sr 487.41 516.87 ppm Y 0.11 0.12 ppm Cs -0.01 0.00 ppm Ba 88.42 90.79 ppm La 0.59 0.69 ppm Ce 1.30 1.41 ppm Pr 0.11 0.12 ppm Nd 0.47 0.42 ppm Sm 0.08 0.08 ppm Eu 0.26 0.25 ppm Gd 0.05 0.04 ppm Tb 0.00 0.01 ppm Pb 0.65 0.66

155 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B GR-31-B mineral pppp c/i/r riic Line Numbers 152 153 154 155 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 14.12 13.25 13.55 10.03 K2O 0.14 0.19 0.22 0.49 SiO2 49.82 50.41 49.99 54.39 Al2O3 31.39 31.30 31.17 28.08 FeO 0.45 0.81 0.61 0.63 Na2O 4.20 4.29 4.15 5.81 BaO -0.05 0.03 -0.01 0.07 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.1 100.3 99.7 99.5 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

156 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B GR-31-B mineral pppp c/i/r iirr Line Numbers 156 157 158 159 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 11.61 13.28 12.65 13.80 K2O 0.32 0.25 0.28 0.12 SiO2 52.51 50.15 51.24 49.70 Al2O3 29.08 31.00 30.09 31.26 FeO 0.55 0.60 0.63 0.46 Na2O 5.18 4.25 4.70 4.07 BaO -0.02 0.03 -0.06 0.02 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.2 99.6 99.5 99.4 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

157 Unit Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B mineral ppp c/i/r Line Numbers 160 Un 13 G 176 177 Un 15 G 7/13/2009 7/13/2009 7/13/2009 CaO 13.67 13.16 13.30 K2O 0.18 0.27 0.17 SiO2 50.41 50.93 50.72 Al2O3 30.78 29.73 29.97 FeO 0.56 0.65 0.68 Na2O 4.33 4.75 4.78 BaO 0.05 TiO2 0.00 0.04 0.07 MgO 0.00 0.18 0.28 MnO 0.00 0.01 0.01 Oxide Totals 100.0 99.7 100.0 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

158 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B GR-31-B mineral pppp c/i/r riic Line Numbers 181 182 183 184 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.02 13.19 13.02 13.50 K2O 0.22 0.16 0.16 0.14 SiO2 50.58 50.69 50.57 50.25 Al2O3 30.50 30.30 30.38 30.66 FeO 0.57 0.58 0.59 0.48 Na2O 4.68 4.47 4.64 4.39 BaO 0.01 0.08 0.05 -0.01 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.6 99.5 99.4 99.4 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

159 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B GR-31-B mineral pppp c/i/r ciir Line Numbers 185 186 187 188 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.25 13.11 13.26 12.79 K2O 0.13 0.17 0.24 0.28 SiO2 49.98 49.90 50.41 50.24 Al2O3 30.79 30.48 30.58 30.36 FeO 0.53 0.50 0.61 0.69 Na2O 4.32 4.50 4.53 4.88 BaO 0.01 -0.03 0.00 -0.07 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.0 98.6 99.6 99.2 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

160 Unit Gardiner River Gardiner River Gardiner River Sample GR-31-B GR-31-B GR-31-B mineral ppp c/i/r ric Line Numbers Un 19 G 199 200 201 7/13/2009 7/13/2009 7/13/2009 CaO 12.95 11.11 11.78 K2O 0.25 0.27 0.31 SiO2 50.75 54.25 52.90 Al2O3 29.61 28.52 28.48 FeO 0.52 0.46 1.06 Na2O 4.49 5.66 5.12 BaO -0.01 0.05 0.06 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 98.5 100.3 99.7 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

161 Unit Gardiner River Gardiner River Grizzly Lake Grizzly Lake Sample GR-31-B GR-31-B GL 4B GL 4B mineral pp pp c/i/r ir rc Line Numbers 204 212 Un 28 G 169 171 7/13/2009 7/13/2009 4/29/2009 4/29/2009 CaO 12.05 13.71 14.40 13.55 K2O 0.34 0.14 0.14 0.14 SiO2 52.24 51.12 50.51 51.65 Al2O3 28.08 30.52 30.98 29.99 FeO 1.40 0.43 0.80 0.77 Na2O 4.88 4.24 3.21 3.66 BaO -0.01 0.05 0.00 0.00 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.0 100.2 100.0 99.8 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

162 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral pppp c/i/r ccrc Line Numbers Un 31 G 177 179 180 181 4/29/2009 4/29/2009 4/29/2009 4/29/2009 CaO 13.92 13.73 9.17 13.61 K2O 0.09 0.12 0.47 0.13 SiO2 50.78 51.30 56.28 51.75 Al2O3 30.33 29.93 25.95 29.85 FeO 0.74 0.85 1.47 0.83 Na2O 3.20 3.40 5.79 3.62 BaO 0.15 0.12 0.13 0.15 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.2 99.4 99.3 99.9 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

163 Unit Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B mineral ppp c/i/r c Line Numbers 182 Un 22 GL 224 Un 23 GL 227 4/29/2009 7/13/2009 7/13/2009 CaO 13.86 13.63 13.92 K2O 0.09 0.07 0.09 SiO2 51.27 50.55 50.08 Al2O3 30.25 30.53 30.85 FeO 0.75 0.57 0.49 Na2O 3.39 3.88 3.88 BaO 0.20 0.03 0.04 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 99.8 99.3 99.4 ppm Ti 444.96 ppm Rb 0.42 ppm Sr 483.60 ppm Y 0.63 ppm Cs 0.01 ppm Ba 41.38 ppm La 1.08 ppm Ce 1.70 ppm Pr 0.21 ppm Nd 0.93 ppm Sm 0.19 ppm Eu 0.27 ppm Gd 0.16 ppm Tb 0.02 ppm Pb 3.84

164 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral pp p p c/i/r Line Numbers 228 229 230 231 Un 24 GL 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 12.84 13.09 13.22 13.46 K2O 0.19 0.15 0.24 0.18 SiO2 51.31 51.41 50.29 50.76 Al2O3 29.56 30.28 29.33 29.92 FeO 0.60 0.55 0.65 0.61 Na2O 4.46 4.23 4.31 4.17 BaO 0.09 0.04 0.02 0.01 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.0 99.7 98.1 99.1 ppm Ti 457.26 681.73 ppm Rb 0.36 0.65 ppm Sr 446.98 499.22 ppm Y 0.30 0.82 ppm Cs 0.01 0.01 ppm Ba 37.68 44.13 ppm La 0.72 1.42 ppm Ce 1.38 2.52 ppm Pr 0.14 0.32 ppm Nd 0.58 1.27 ppm Sm 0.12 0.26 ppm Eu 0.26 0.27 ppm Gd 0.10 0.22 ppm Tb 0.01 0.03 ppm Pb 1.64 10.42

165 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral ss ss c/i/r rr cc Line Numbers 232 233 Un 25 GL 234 235 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 1.18 0.57 0.82 1.64 K2O 7.87 10.15 9.33 7.45 SiO2 65.88 65.21 64.18 66.54 Al2O3 18.99 19.01 18.27 19.03 FeO 0.19 0.12 0.37 0.23 Na2O 6.00 5.24 5.14 5.91 BaO 0.02 0.12 0.14 0.04 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.1 100.4 98.2 100.8 A - rim B - core ppm Ti 79.95 72.57 ppm Rb 161.19 130.08 ppm Sr 69.88 45.85 ppm Y 0.43 0.35 ppm Cs 0.14 0.10 ppm Ba 640.46 667.86 ppm La 2.47 2.23 ppm Ce 2.77 2.38 ppm Pr 0.16 0.13 ppm Nd 0.47 0.41 ppm Sm 0.09 0.07 ppm Eu 1.30 1.25 ppm Gd 0.08 0.07 ppm Tb 0.01 0.01 ppm Pb 33.70 31.50

166 Unit Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B mineral ppp c/i/r Line Numbers Un 26 GL 237 Un 27 GL 241 242 7/13/2009 7/13/2009 7/13/2009 CaO 13.57 3.75 3.23 K2O 0.12 3.11 4.72 SiO2 50.95 62.97 64.04 Al2O3 30.47 20.97 21.13 FeO 0.60 0.23 0.26 Na2O 4.20 8.40 7.06 BaO -0.01 0.04 0.05 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 99.9 99.5 100.5 light dark ppm Ti 443.90 631.35 ppm Rb 0.33 0.64 ppm Sr 452.01 424.21 ppm Y 0.24 0.55 ppm Cs 0.00 0.01 ppm Ba 40.80 38.60 ppm La 0.69 0.99 ppm Ce 1.55 2.16 ppm Pr 0.14 0.26 ppm Nd 0.67 1.04 ppm Sm 0.11 0.27 ppm Eu 0.27 0.27 ppm Gd 0.08 0.23 ppm Tb 0.01 0.03 ppm Pb 4.26 5.01

167 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral p ppp c/i/r rri Line Numbers 243 Un 28 GL 244 245 246 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 2.84 6.39 2.93 2.52 K2O 2.69 2.04 3.66 3.90 SiO2 64.01 62.29 64.42 63.73 Al2O3 21.26 21.38 21.44 20.85 FeO 0.24 1.33 0.18 0.21 Na2O 9.29 5.45 8.43 8.33 BaO 0.11 0.06 0.10 0.13 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.4 98.9 101.2 99.7 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

168 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B GL 4B mineral ppppp c/i/r iiiic Line Numbers 247 248 249 251 253 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 3.51 2.90 4.61 3.96 3.64 K2O 1.82 2.10 1.22 1.40 2.20 SiO2 63.60 63.00 62.73 61.43 62.61 Al2O3 22.19 21.50 23.08 22.52 22.35 FeO 0.19 0.20 0.17 0.22 0.21 Na2O 9.44 9.27 9.58 9.29 9.03 BaO 0.12 0.21 0.22 0.10 0.10 TiO2 0.00 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 0.00 Oxide Totals 100.9 99.2 101.6 98.9 100.1 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

169 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral ppp p c/i/r ccc c Line Numbers 254 255 256 257 Un 29 GL 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 3.68 3.83 3.37 4.19 K2O 1.46 1.53 1.68 2.01 SiO2 62.26 62.74 62.77 61.72 Al2O3 22.31 22.38 21.96 22.29 FeO 0.17 0.18 0.20 0.21 Na2O 9.41 9.46 9.76 8.82 BaO 0.05 0.07 0.07 0.08 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.3 100.2 99.8 99.3 ppm Ti 57.93 ppm Rb 5.90 ppm Sr 128.79 ppm Y 0.10 ppm Cs -0.01 ppm Ba 442.84 ppm La 7.29 ppm Ce 9.09 ppm Pr 0.60 ppm Nd 1.52 ppm Sm 0.16 ppm Eu 3.04 ppm Gd 0.06 ppm Tb 0.00 ppm Pb 14.57

170 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral pp p p c/i/r r Line Numbers 259 260 262 Un 56 GL 428 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 12.68 12.90 12.98 11.72 K2O 0.21 0.19 0.15 0.27 SiO2 51.35 51.31 51.54 52.66 Al2O3 29.40 29.64 29.60 28.92 FeO 0.63 0.64 0.60 0.89 Na2O 4.58 4.51 4.53 4.70 BaO 0.11 -0.01 0.00 0.00 TiO2 0.00 0.00 0.00 0.06 MgO 0.00 0.00 0.00 0.22 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.0 99.2 99.4 99.4 ppm Ti 461.67 ppm Rb 0.36 ppm Sr 446.51 ppm Y 0.12 ppm Cs 0.00 ppm Ba 38.79 ppm La 0.61 ppm Ce 1.30 ppm Pr 0.13 ppm Nd 0.39 ppm Sm 0.08 ppm Eu 0.26 ppm Gd 0.06 ppm Tb 0.01 ppm Pb 2.87

171 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B GL 4B mineral ppppp c/i/r riiii Line Numbers 429 430 431 433 434 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.30 13.77 13.78 13.72 13.66 K2O 0.11 0.09 0.09 0.10 0.09 SiO2 50.93 50.14 50.66 50.64 50.94 Al2O3 31.14 31.23 31.07 31.21 30.92 FeO 0.43 0.40 0.40 0.43 0.40 Na2O 3.67 3.60 3.65 3.71 3.70 BaO 0.00 0.00 0.00 0.00 0.00 TiO2 0.01 0.04 0.00 0.02 0.02 MgO 0.20 0.19 0.21 0.27 0.17 MnO 0.02 0.01 0.05 0.02 0.00 Oxide Totals 99.8 99.5 99.9 100.1 99.9 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

172 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B GL 4B mineral ppppp c/i/r i iccc Line Numbers 435 436 437 439 442 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.54 13.36 13.56 13.87 13.42 K2O 0.10 0.11 0.12 0.10 0.17 SiO2 51.24 50.70 51.24 50.76 51.67 Al2O3 31.11 30.66 30.64 30.89 30.64 FeO 0.47 0.41 0.42 0.42 0.53 Na2O 3.66 3.86 3.81 3.74 3.91 BaO 0.00 0.00 0.00 0.00 0.00 TiO2 0.02 0.01 0.01 0.04 0.07 MgO 0.20 0.19 0.20 0.20 0.21 MnO 0.00 0.00 0.00 0.01 0.00 Oxide Totals 100.3 99.3 100.0 100.0 100.6 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

173 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B GL 4B mineral ppppp c/i/r ccccc Line Numbers 443 444 445 446 447 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.31 13.76 12.56 13.88 13.88 K2O 0.14 0.11 0.09 0.09 0.10 SiO2 51.89 50.92 45.90 51.02 50.28 Al2O3 30.23 30.93 28.04 31.18 31.37 FeO 0.52 0.45 0.54 0.41 0.45 Na2O 3.96 3.73 3.40 3.65 3.59 BaO 0.00 0.00 0.00 0.00 0.00 TiO2 0.04 0.02 0.06 0.03 0.03 MgO 0.20 0.17 0.18 0.15 0.17 MnO 0.01 0.00 0.12 0.00 0.03 Oxide Totals 100.3 100.1 90.9 100.4 99.9 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

174 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B GL 4B mineral ppppp c/i/r ciiii Line Numbers 448 449 450 451 452 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.27 13.79 13.53 13.62 13.69 K2O 0.16 0.12 0.11 0.13 0.12 SiO2 51.37 50.41 50.50 50.90 50.95 Al2O3 29.60 31.09 30.70 31.39 30.88 FeO 1.21 0.45 0.57 0.44 0.53 Na2O 3.79 3.62 3.68 3.64 3.78 BaO 0.00 0.00 0.00 0.00 0.00 TiO2 0.04 0.02 0.04 -0.01 0.02 MgO 0.58 0.25 0.25 0.17 0.19 MnO 0.05 0.00 0.04 0.03 0.00 Oxide Totals 100.1 99.7 99.4 100.3 100.2 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

175 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B GL 4B mineral ppppp c/i/r iiiii Line Numbers 453 454 455 456 457 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.52 13.77 13.50 13.40 13.64 K2O 0.09 0.11 0.08 0.13 0.09 SiO2 51.25 51.11 51.16 51.14 51.42 Al2O3 31.13 30.05 31.11 30.59 30.91 FeO 0.41 0.60 0.41 0.47 0.46 Na2O 3.78 3.67 3.81 3.69 3.83 BaO 0.00 0.00 0.00 0.00 0.00 TiO2 0.05 0.02 0.04 0.03 0.09 MgO 0.16 0.17 0.17 0.20 0.21 MnO 0.02 0.04 0.00 0.02 0.01 Oxide Totals 100.4 99.5 100.3 99.7 100.7 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

176 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 4B GL 4B GL 4B GL 4B mineral pppp c/i/r irrr Line Numbers 458 459 460 461 Un 61 G 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.70 13.90 13.79 13.57 K2O 0.13 0.09 0.13 0.08 SiO2 51.18 50.88 50.81 51.01 Al2O3 30.71 30.94 30.91 31.23 FeO 0.43 0.44 0.40 0.42 Na2O 3.79 3.63 3.59 3.56 BaO 0.00 0.00 0.00 0.00 TiO2 0.02 0.03 0.01 0.03 MgO 0.18 0.20 0.17 0.14 MnO 0.03 0.06 0.02 0.04 Oxide Totals 100.2 100.2 99.8 100.1 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

177 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral ssss c/i/r rrrr Line Numbers 491 492 493 494 Un 62 G 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 0.46 0.47 0.47 0.27 K2O 8.29 8.40 8.53 8.56 SiO2 66.33 66.00 65.65 65.85 Al2O3 19.40 19.60 19.43 19.21 FeO 0.12 0.18 0.17 0.18 Na2O 5.73 5.73 5.73 5.76 BaO 0.08 0.18 0.09 0.12 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.4 100.6 100.1 100.0 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

178 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral ss s s c/i/r cc c r Line Numbers 495 496 497 Un 63 G 498 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 0.36 0.38 0.32 0.41 K2O 8.88 8.55 8.51 8.75 SiO2 65.84 66.07 65.80 65.05 Al2O3 19.49 19.47 19.46 19.39 FeO 0.11 0.16 0.18 0.22 Na2O 5.46 5.51 5.60 5.49 BaO 0.14 0.11 0.02 0.15 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.3 100.3 99.9 99.5 ppm Ti 445.86 ppm Rb 0.35 ppm Sr 465.42 ppm Y 0.11 ppm Cs 0.00 ppm Ba 38.14 ppm La 0.66 ppm Ce 1.51 ppm Pr 0.13 ppm Nd 0.41 ppm Sm 0.08 ppm Eu 0.23 ppm Gd 0.04 ppm Tb 0.01 ppm Pb 0.62

179 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral sss s c/i/r rrr c Line Numbers 499 500 501 Un 65 G 512 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 0.39 0.38 0.54 0.40 K2O 8.77 8.89 8.44 9.01 SiO2 65.77 65.87 66.23 66.28 Al2O3 19.42 19.48 19.49 19.35 FeO 0.13 0.13 0.11 0.11 Na2O 5.55 5.50 5.60 5.37 BaO 0.10 0.11 0.07 0.15 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.1 100.4 100.5 100.7 rim ppm Ti 89.13 ppm Rb 101.29 ppm Sr 42.96 ppm Y 0.85 ppm Cs 0.07 ppm Ba 981.54 ppm La 4.11 ppm Ce 5.04 ppm Pr 0.32 ppm Nd 0.84 ppm Sm 0.16 ppm Eu 1.54 ppm Gd 0.14 ppm Tb 0.03 ppm Pb 39.37

180 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral ss pp c/i/r cc rr Line Numbers 513 514 Un 68 G 521 522 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 0.41 0.49 13.75 13.40 K2O 9.11 8.23 0.13 0.18 SiO2 65.49 65.91 50.66 51.17 Al2O3 19.68 19.87 30.79 30.98 FeO 0.14 0.11 0.65 0.58 Na2O 5.52 5.94 3.66 3.77 BaO 0.15 0.13 0.02 0.06 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.5 100.7 99.7 100.1 core ppm Ti 81.59 ppm Rb 100.44 ppm Sr 41.05 ppm Y 1.76 ppm Cs 0.07 ppm Ba 716.46 ppm La 5.11 ppm Ce 4.24 ppm Pr 0.38 ppm Nd 1.01 ppm Sm 0.31 ppm Eu 1.28 ppm Gd 0.26 ppm Tb 0.09 ppm Pb 32.86

181 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral pp p p c/i/r rr c c Line Numbers 523 524 Un 69 GL 525 526 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.62 13.60 13.54 13.48 K2O 0.16 0.15 0.12 0.12 SiO2 51.09 50.90 51.14 51.53 Al2O3 30.35 30.68 31.04 30.38 FeO 0.54 0.56 0.63 0.55 Na2O 3.79 3.76 3.81 3.82 BaO 0.01 0.03 0.00 0.03 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 99.6 99.7 100.3 99.9 ppm Ti 674.98 ppm Rb 0.89 ppm Sr 541.06 ppm Y 0.80 ppm Cs 0.00 ppm Ba 63.26 ppm La 1.46 ppm Ce 3.38 ppm Pr 0.45 ppm Nd 1.28 ppm Sm 0.22 ppm Eu 0.33 ppm Gd 0.14 ppm Tb 0.03 ppm Pb 8.85

182 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral pp pp c/i/r cc Line Numbers 527 528 Un 71 GL 531 532 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.55 13.14 14.32 14.41 K2O 0.09 0.16 0.10 0.09 SiO2 50.95 51.64 50.64 50.57 Al2O3 30.71 30.34 30.59 30.57 FeO 0.64 0.53 0.47 0.53 Na2O 3.96 3.91 3.45 3.45 BaO 0.02 0.00 TiO2 0.00 0.00 0.03 0.02 MgO 0.00 0.00 0.20 0.21 MnO 0.00 0.00 0.04 0.04 Oxide Totals 99.9 99.7 99.8 99.9 ppm Ti 431.12 ppm Rb 0.53 ppm Sr 465.66 ppm Y 0.32 ppm Cs 0.00 ppm Ba 52.21 ppm La 0.93 ppm Ce 2.09 ppm Pr 0.17 ppm Nd 3.56 ppm Sm 0.12 ppm Eu 0.24 ppm Gd 0.06 ppm Tb 0.01 ppm Pb 3.11

183 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral pp pp c/i/r rr Line Numbers 533 534 Un 73 G 538 539 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 14.09 14.18 13.48 13.72 K2O 0.13 0.14 0.12 0.15 SiO2 50.97 50.62 50.85 50.71 Al2O3 30.34 30.68 30.85 30.98 FeO 0.54 0.49 0.61 0.83 Na2O 3.62 3.65 3.75 3.77 BaO 0.07 0.00 TiO2 0.10 0.05 0.00 0.00 MgO 0.23 0.18 0.00 0.00 MnO 0.03 0.02 0.00 0.00 Oxide Totals 100.0 100.0 99.7 100.1 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

184 Unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Sample GL 5B GL 5B GL 5B GL 5B mineral pppp c/i/r rccc Line Numbers 540 Un 74 GL 541 542 543 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.38 13.66 13.55 13.85 K2O 0.13 0.12 0.17 0.11 SiO2 51.27 50.99 51.61 50.49 Al2O3 31.06 30.95 30.79 31.16 FeO 0.72 0.57 0.60 0.55 Na2O 3.62 3.74 3.80 3.69 BaO 0.00 0.03 0.00 0.00 TiO2 0.00 0.00 0.00 0.00 MgO 0.00 0.00 0.00 0.00 MnO 0.00 0.00 0.00 0.00 Oxide Totals 100.2 100.0 100.5 99.8 ppm Ti 430.44 ppm Rb 0.92 ppm Sr 407.91 ppm Y 0.35 ppm Cs 0.00 ppm Ba 44.64 ppm La 0.86 ppm Ce 2.41 ppm Pr 0.22 ppm Nd 0.64 ppm Sm 0.14 ppm Eu 0.22 ppm Gd 0.11 ppm Tb 0.02 ppm Pb 5.96

185 Unit Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 mineral ppp c/i/r rrr Line Numbers Un 98 GR 721 722 723 Un 99 GR 7/13/2009 7/13/2009 7/13/2009 CaO 13.23 12.89 12.86 K2O 0.24 0.25 0.23 SiO2 51.37 51.79 51.52 Al2O3 30.83 30.38 30.37 FeO 0.67 0.85 0.75 Na2O 3.93 4.19 3.93 BaO 0.00 0.04 0.00 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 100.3 100.4 99.6 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

186 Unit Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 mineral ppp c/i/r ccc Line Numbers 724 725 726 Un 109 G 7/13/2009 7/13/2009 7/13/2009 CaO 13.34 13.31 13.13 K2O 0.17 0.19 0.18 SiO2 50.92 51.10 51.75 Al2O3 31.03 30.73 30.71 FeO 0.53 0.56 0.60 Na2O 3.82 3.81 3.99 BaO 0.08 0.00 0.00 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 99.9 99.7 100.3 ppm Ti 451.89 ppm Rb 0.45 ppm Sr 566.37 ppm Y 0.17 ppm Cs 0.00 ppm Ba 69.46 ppm La 0.84 ppm Ce 1.61 ppm Pr 0.13 ppm Nd 0.44 ppm Sm 0.14 ppm Eu 0.26 ppm Gd 0.03 ppm Tb 0.00 ppm Pb 1.18

187 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 GR-1 mineral pppp c/i/r Line Numbers 767 768 769 770 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.63 13.70 12.87 7.90 K2O 0.14 0.17 0.15 1.92 SiO2 51.05 50.81 51.78 57.66 Al2O3 31.25 31.06 30.26 15.63 FeO 0.50 0.49 0.56 4.91 Na2O 3.69 3.60 4.17 3.86 BaO 0.00 0.00 0.00 0.00 TiO2 0.04 0.00 0.04 0.24 MgO 0.18 0.17 0.20 2.39 MnO 0.03 0.00 0.00 0.17 Oxide Totals 100.5 100.0 100.0 94.7 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

188 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 GR-1 mineral pppp c/i/r Line Numbers 771 772 773 774 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.56 13.56 13.76 13.68 K2O 0.13 0.16 0.16 0.14 SiO2 51.01 50.89 51.28 50.67 Al2O3 30.71 31.20 31.15 30.67 FeO 0.52 0.53 0.53 0.58 Na2O 3.78 3.80 3.64 3.86 BaO 0.00 0.00 0.00 0.00 TiO2 0.00 0.02 0.07 0.05 MgO 0.18 0.21 0.22 0.20 MnO 0.01 0.00 0.04 0.03 Oxide Totals 99.9 100.3 100.8 99.9 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

189 Unit Gardiner River Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 GR-1 mineral pppp c/i/r Line Numbers 775 776 777 778 7/13/2009 7/13/2009 7/13/2009 7/13/2009 CaO 13.50 13.41 12.76 12.85 K2O 0.12 0.18 0.19 0.18 SiO2 51.56 51.45 52.01 52.46 Al2O3 31.07 30.62 30.06 30.01 FeO 0.52 0.56 0.56 0.49 Na2O 3.79 3.66 4.10 4.17 BaO 0.00 0.00 0.00 0.00 TiO2 0.04 0.00 0.02 0.00 MgO 0.17 0.16 0.13 0.18 MnO 0.00 0.03 0.00 0.00 Oxide Totals 100.7 100.1 99.8 100.3 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

190 Unit Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 mineral ppp c/i/r rr Line Numbers 779 Un 110 GR 780 781 7/13/2009 7/13/2009 7/13/2009 CaO 13.13 10.00 13.55 K2O 0.16 0.36 0.23 SiO2 51.74 55.12 51.23 Al2O3 30.47 27.82 31.09 FeO 0.61 0.76 0.56 Na2O 3.97 5.74 3.60 BaO 0.00 0.00 0.08 TiO2 0.05 0.00 0.00 MgO 0.21 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 100.3 99.8 100.3 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

191 Unit Gardiner River Gardiner Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 GR-1 mineral ppp c/i/r rcc Line Numbers 782 Un 111 G 783 784 7/13/2009 7/13/2009 7/13/2009 CaO 13.00 13.85 12.90 K2O 0.25 0.09 0.22 SiO2 51.76 51.01 51.82 Al2O3 30.55 31.25 30.44 FeO 0.63 0.37 0.52 Na2O 3.93 3.65 3.91 BaO 0.00 0.09 0.00 TiO2 0.00 0.00 0.00 MgO 0.00 0.00 0.00 MnO 0.00 0.00 0.00 Oxide Totals 100.1 100.3 99.7 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

192 Unit Gardiner River Gardiner River Crystal Springs Sample GR-1 GR-1 08CP69C mineral pp p c/i/r cc Line Numbers 785 786 Un 32 08 267 7/13/2009 7/13/2009 11/9/2009 CaO 12.97 12.72 12.97 K2O 0.19 0.15 0.09 SiO2 51.98 51.67 52.06 Al2O3 30.45 30.57 30.58 FeO 0.43 0.50 0.60 Na2O 4.14 3.95 3.73 BaO 0.05 0.00 0.04 TiO2 0.00 0.00 MgO 0.00 0.00 MnO 0.00 0.00 Oxide Totals 100.2 99.6 100.1 ppm Ti 382.83 ppm Rb 0.24 ppm Sr 543.16 ppm Y 0.18 ppm Cs 0.00 ppm Ba 62.81 ppm La 0.66 ppm Ce 1.44 ppm Pr 0.11 ppm Nd 0.41 ppm Sm 0.10 ppm Eu 0.27 ppm Gd 0.06 ppm Tb 0.00 ppm Pb 0.49

193 Unit Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C mineral ppp c/i/r Line Numbers 268 269 270 Un 33 0 11/10/2009 11/11/2009 11/12/2009 CaO 13.11 13.27 13.22 K2O 0.09 0.10 0.11 SiO2 51.58 51.595886 51.283131 Al2O3 30.56 30.614098 30.250183 FeO 0.63 0.609602 0.788894 Na2O 3.74 3.67216 3.746448 BaO 0.00 0 0.007326 TiO2 MgO MnO Oxide Totals 99.7 99.9 99.4 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

194 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 271 272 273 274 11/14/2009 11/15/2009 11/16/2009 11/17/2009 CaO 13.92 13.92 12.92 12.89 K2O 0.07 0.12 0.13 0.14 SiO2 50.373631 51.007607 51.595058 51.633221 Al2O3 31.222757 31.058834 29.966293 30.456932 FeO 0.58171 0.696211 0.662394 0.656893 Na2O 3.232638 3.34191 3.602523 3.838196 BaO 0000 TiO2 MgO MnO Oxide Totals 99.4 100.2 98.9 99.6 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

195 Unit Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C mineral pp p c/i/r Line Numbers 275 276 Un 36 08C 309 11/18/2009 11/19/2009 11/21/2009 CaO 13.52 13.24 13.64 K2O 0.12 0.12 0.09 SiO2 51.618587 51.131485 50.946011 Al2O3 30.438557 31.271399 30.932726 FeO 0.617422 0.683295 0.717524 Na2O 3.668908 3.609604 3.511711 BaO 0 0 0.021985 TiO2 MgO MnO Oxide Totals 100.0 100.1 99.9 51 ppm Ti 1176.08 ppm Rb 3.90 ppm Sr 379.28 ppm Y 3.99 ppm Cs 0.11 ppm Ba 46.28 ppm La 2.91 ppm Ce 6.38 ppm Pr 1.01 ppm Nd 3.48 ppm Sm 0.95 ppm Eu 0.34 ppm Gd 0.69 ppm Tb 0.15 ppm Pb 4.30

196 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 310 311 312 313 11/22/2009 11/23/2009 11/24/2009 11/25/2009 CaO 13.56 13.15 13.55 13.23 K2O 0.08 0.10 0.11 0.12 SiO2 51.023582 51.958969 51.419491 51.82291 Al2O3 30.853609 30.479038 30.966066 30.825712 FeO 0.527511 0.58643 0.582915 0.643164 Na2O 3.448222 3.753709 3.545283 3.820002 BaO 0.040842 0 0 0 TiO2 MgO MnO Oxide Totals 99.5 100.0 100.2 100.5 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

197 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 314 315 316 317 11/26/2009 11/27/2009 11/28/2009 11/29/2009 CaO 13.61 13.27 13.41 13.45 K2O 0.11 0.14 0.10 0.11 SiO2 51.360615 51.796978 51.655228 51.587891 Al2O3 30.856709 29.93071 30.738533 30.849033 FeO 0.658936 1.062927 0.540265 0.54048 Na2O 3.482454 3.771608 3.487228 3.65376 BaO 0 0 0.00944 0 TiO2 MgO MnO Oxide Totals 100.1 100.0 99.9 100.2 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

198 Unit Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C mineral ppp c/i/r Line Numbers 318 Un 38 0 327 328 11/30/2009 12/2/2009 12/3/2009 CaO 13.29 14.61 13.09 K2O 0.09 0.02 0.13 SiO2 51.693844 49.612263 51.730545 Al2O3 30.182228 31.882113 30.46011 FeO 0.746478 0.473759 0.724105 Na2O 3.720364 2.877761 3.725976 BaO 0.008388 0.003148 0 TiO2 MgO MnO Oxide Totals 99.7 99.5 99.9 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

199 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 329 330 331 332 12/4/2009 12/5/2009 12/6/2009 12/7/2009 CaO 13.03 12.99 13.39 13.20 K2O 0.13 0.10 0.12 0.13 SiO2 52.243992 52.395325 51.848213 51.584812 Al2O3 30.226 30.295946 30.709955 29.977249 FeO 0.809004 0.524778 0.684242 0.764072 Na2O 4.070983 3.959898 3.525715 3.780606 BaO 0 0.023071 0.026213 0.002096 TiO2 MgO MnO Oxide Totals 100.5 100.3 100.3 99.4 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

200 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 333 334 335 336 12/8/2009 12/9/2009 12/10/2009 12/11/2009 CaO 13.15 13.60 12.99 13.35 K2O 0.10 0.09 0.12 0.12 SiO2 52.233856 50.579308 51.794868 51.491024 Al2O3 30.384295 30.830088 30.447998 30.649254 FeO 0.721038 0.911488 0.726304 0.740232 Na2O 3.66243 3.367301 3.882258 3.607907 BaO 0 0.030396 0.059741 0.010482 TiO2 MgO MnO Oxide Totals 100.3 99.4 100.0 100.0 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

201 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 337 338 339 341 12/12/2009 12/13/2009 12/14/2009 12/16/2009 CaO 13.81 12.89 13.90 13.13 K2O 0.09 0.13 0.10 0.19 SiO2 50.939598 52.459892 50.675922 52.275707 Al2O3 31.207422 30.231279 31.210424 30.428537 FeO 0.580908 0.680563 0.519536 0.73519 Na2O 3.436946 3.787719 3.300069 3.738427 BaO 0.056622 0 0 0.017825 TiO2 MgO MnO Oxide Totals 100.1 100.2 99.7 100.5 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

202 Unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs Sample 08CP69C 08CP69C 08CP69C 08CP69C mineral pppp c/i/r Line Numbers 342 343 344 345 12/17/2009 12/18/2009 12/19/2009 12/20/2009 CaO 13.94 13.37 13.35 13.68 K2O 0.16 0.16 0.17 0.12 SiO2 50.758205 51.538212 51.401569 50.612041 Al2O3 31.18498 30.51325 30.930201 31.125834 FeO 0.707476 0.718097 0.745359 0.649256 Na2O 3.284827 3.904999 3.650654 3.363331 BaO 0 0 0.04392 0 TiO2 MgO MnO Oxide Totals 100.0 100.2 100.3 99.6 ppm Ti ppm Rb ppm Sr ppm Y ppm Cs ppm Ba ppm La ppm Ce ppm Pr ppm Nd ppm Sm ppm Eu ppm Gd ppm Tb ppm Pb

203

APPENDIX D

RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF XENOCRYSTS FROM THE MINGLED MAGMAS

Unit Grizzly Lake Grizzly Lake Grizzly Lake Sample GL-4B GL-4B GL-4B mineral c/i/r Line Numbers Un 26 G 167 Un 27 GL 4B 168 Un 30 G 176 4/29/2009 4/29/2009 4/29/2009 4/29/2009 FeO Oxide Percents 0.29 0.28 0.23 TiO2 Oxide Percents 0.11 0.00 0.04 CaO Oxide Percents 0.00 0.04 0.06 SiO2 Oxide Percents 97.46 97.42 98.70 Al2O3 Oxide Percents 1.30 1.28 0.66 K2O Oxide Percents 0.25 0.23 0.14 Na2O Oxide Percents 0.14 0.09 0.11 BaO Oxide Percents 0.00 0.14 0.00 MgO Oxide Percents 0.00 0.00 0.00 MnO Oxide Percents 0.00 0.00 0.01 Oxide Totals 99.55 99.49 99.95

Sc45(LR) Ti47(LR) Rb85(LR) Sr88(LR) Y89(LR) Zr90(LR) Nb93(LR) Cs133(LR) Ba138(LR) La139(LR) Ce140(LR) Pr141(LR) Nd146(LR) Sm147(LR) Eu151(LR) Gd160(LR) Tb159(LR) Dy163(LR) Ho165(LR) Er166(LR) Tm169(LR) Yb172(LR) Lu175(LR) Hf178(LR) Ta181(LR) Pb208(LR) Th232(LR) U238(LR)

205 Unit Gardiner River Gardiner River Gardiner River Gardiner Rive Gardiner River Sample GR-1 GR-1 GR-1 GR-1 GR-1 mineral c/i/r Line Numbers Un 102 G 740 742 743 Un 104 GR 748 749 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 FeO Oxide Percents 1.34 0.27 0.47 0.59 0.50 TiO2 Oxide Percents 0.00 0.00 0.00 0.00 0.00 CaO Oxide Percents 4.47 4.88 6.27 6.22 5.12 SiO2 Oxide Percents 62.92 62.38 60.96 60.33 65.84 Al2O3 Oxide Percents 21.77 23.94 23.69 24.29 20.30 K2O Oxide Percents 2.53 1.07 0.65 0.85 0.65 Na2O Oxide Percents 6.71 8.13 7.12 7.34 6.48 BaO Oxide Percents 0.00 0.15 0.00 0.08 0.00 MgO Oxide Percents 0.00 0.00 0.00 0.00 0.00 MnO Oxide Percents 0.00 0.00 0.00 0.00 0.00 Oxide Totals 99.75 100.82 99.16 99.10 98.40

Sc45(LR) 3.25 3.43 Ti47(LR) 406.95 610.54 Rb85(LR) 24.09 12.15 Sr88(LR) 159.53 176.79 Y89(LR) 7.56 5.59 Zr90(LR) 20.16 18.20 Nb93(LR) 8.19 5.55 Cs133(LR) 0.29 0.51 Ba138(LR) 382.84 442.88 La139(LR) 17.18 12.87 Ce140(LR) 34.54 26.57 Pr141(LR) 2.75 2.19 Nd146(LR) 10.17 7.15 Sm147(LR) 1.77 1.32 Eu151(LR) 1.35 1.53 Gd160(LR) 1.37 1.04 Tb159(LR) 0.22 0.17 Dy163(LR) 1.42 1.04 Ho165(LR) 0.28 0.22 Er166(LR) 0.76 0.62 Tm169(LR) 0.10 0.09 Yb172(LR) 0.61 0.54 Lu175(LR) 0.10 0.06 Hf178(LR) 0.70 0.58 Ta181(LR) 0.32 0.26 Pb208(LR) 24.14 21.39 Th232(LR) 3.33 3.17 U238(LR) 1.36 0.95

206 Unit Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 mineral c/i/r Line Numbers Un 107 G 761 762 763 7/13/2009 7/13/2009 7/13/2009 FeO Oxide Percents 0.70 0.27 0.23 TiO2 Oxide Percents 0.05 0.02 0.00 CaO Oxide Percents 4.99 5.62 5.46 SiO2 Oxide Percents 61.03 61.05 61.22 Al2O3 Oxide Percents 23.53 24.45 24.35 K2O Oxide Percents 1.16 0.98 0.88 Na2O Oxide Percents 7.93 8.01 8.08 BaO Oxide Percents 0.00 0.00 0.00 MgO Oxide Percents 0.02 0.01 0.02 MnO Oxide Percents 0.00 0.02 0.00 Oxide Totals 98.65 100.15 100.01

Sc45(LR) 2.59 3.16 Ti47(LR) 536.07 211.08 Rb85(LR) 19.41 33.28 Sr88(LR) 197.42 179.16 Y89(LR) 7.28 7.43 Zr90(LR) 21.26 16.67 Nb93(LR) 7.63 6.56 Cs133(LR) 0.24 1.09 Ba138(LR) 395.14 296.62 La139(LR) 18.14 19.97 Ce140(LR) 32.90 34.50 Pr141(LR) 2.72 2.87 Nd146(LR) 9.14 9.94 Sm147(LR) 1.52 1.79 Eu151(LR) 1.54 1.36 Gd160(LR) 1.33 1.38 Tb159(LR) 0.23 0.22 Dy163(LR) 1.42 1.32 Ho165(LR) 0.26 0.25 Er166(LR) 0.78 0.74 Tm169(LR) 0.11 0.10 Yb172(LR) 0.67 0.66 Lu175(LR) 0.11 0.08 Hf178(LR) 0.66 0.79 Ta181(LR) 0.32 0.29 Pb208(LR) 24.73 27.34 Th232(LR) 3.43 2.85 U238(LR) 0.99 0.89

207 Unit Gardiner River Gardiner River Gardiner River Sample GR-1 GR-1 GR-1 mineral c/i/r Line Numbers Un 108 G 764 765 766 7/13/2009 7/13/2009 7/13/2009 FeO Oxide Percents 0.17 0.13 0.20 TiO2 Oxide Percents 0.01 0.00 0.00 CaO Oxide Percents 1.96 2.31 2.17 SiO2 Oxide Percents 65.19 64.65 64.82 Al2O3 Oxide Percents 21.10 21.47 21.10 K2O Oxide Percents 4.25 3.78 4.15 Na2O Oxide Percents 7.36 7.66 7.51 BaO Oxide Percents 0.00 0.00 0.00 MgO Oxide Percents 0.02 0.00 0.00 MnO Oxide Percents 0.02 0.00 0.00 Oxide Totals 99.91 99.86 99.75

Sc45(LR) 2.69 Ti47(LR) 113.70 Rb85(LR) 8.35 Sr88(LR) 212.95 Y89(LR) 2.26 Zr90(LR) 5.61 Nb93(LR) 2.02 Cs133(LR) 0.06 Ba138(LR) 527.82 La139(LR) 10.87 Ce140(LR) 19.70 Pr141(LR) 1.42 Nd146(LR) 4.29 Sm147(LR) 0.66 Eu151(LR) 1.69 Gd160(LR) 0.42 Tb159(LR) 0.06 Dy163(LR) 0.44 Ho165(LR) 0.07 Er166(LR) 0.21 Tm169(LR) 0.03 Yb172(LR) 0.25 Lu175(LR) 0.03 Hf178(LR) 0.28 Ta181(LR) 0.06 Pb208(LR) 19.38 Th232(LR) 0.83 U238(LR) 0.34

208

APPENDIX E

RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF PYROXENE FROM THE MINGLED MAGMAS

unit Grizzley Lake Grizzley Lake Grizzley Lake sample GL-4B GL-4B GL-4B description pyx pyx pyx date 4/29/2009 4/29/2009 4/29/2009 Line Numbers Un 2 GL4 128 Un 13 GL 140 Un 15 G 143

FeO Oxide Percents 8.42 15.30 7.00 TiO2 Oxide Percents 0.46 2.24 0.85 CaO Oxide Percents 16.75 2.88 19.94 SiO2 Oxide Percents 52.24 64.83 53.09 Al2O3 Oxide Percents 2.22 6.92 3.29 MgO Oxide Percents 18.63 3.77 16.28 MnO Oxide Percents 0.18 0.26 0.21 Na2O Oxide Percents 0.24 2.39 0.31 K2O Oxide Percents 0.04 2.07 0.01 BaO Oxide Percents 0.00 0.00 0.00 Oxide Totals 99.18 100.66 100.98

210 unit Grizzley Lake Grizzley Lake sample GL-4B GL-4B description pyx pyx date 4/29/2009 4/29/2009 Line Numbers Un 18 GL 146 Un 19 G 147

FeO Oxide Percents 9.80 8.96 TiO2 Oxide Percents 0.69 1.57 CaO Oxide Percents 16.41 19.45 SiO2 Oxide Percents 54.05 50.67 Al2O3 Oxide Percents 3.15 4.72 MgO Oxide Percents 15.23 14.62 MnO Oxide Percents 0.19 0.17 Na2O Oxide Percents 0.24 0.29 K2O Oxide Percents 0.07 0.00 BaO Oxide Percents 0.00 0.00 Oxide Totals 99.84 100.45

211 unit Grizzley Lake Grizzley Lake Grizzley Lake sample GL-4B GL-4B GL-4B description pyx pyx pyx date 4/29/2009 4/29/2009 4/29/2009 Line Numbers Un 20 GL 148 149 150

FeO Oxide Percents 8.82 8.15 8.41 TiO2 Oxide Percents 1.03 0.97 1.06 CaO Oxide Percents 18.38 19.31 19.69 SiO2 Oxide Percents 51.24 51.04 51.40 Al2O3 Oxide Percents 4.05 3.67 4.00 MgO Oxide Percents 14.94 14.60 15.25 MnO Oxide Percents 0.20 0.16 0.22 Na2O Oxide Percents 0.29 0.23 0.24 K2O Oxide Percents 0.01 0.03 0.00 BaO Oxide Percents 0.00 0.00 0.00 Oxide Totals 98.96 98.17 100.25

212 unit Grizzley Lake Grizzley Lake Grizzley Lake sample GL-5B GL-5B GL-5B description date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 60 G 488 489 490

FeO Oxide Percents 28.57 30.26 28.87 TiO2 Oxide Percents 0.19 0.26 0.22 CaO Oxide Percents 18.69 17.63 18.75 SiO2 Oxide Percents 47.96 47.94 47.83 Al2O3 Oxide Percents 0.79 0.59 0.53 MgO Oxide Percents 2.15 2.36 2.07 MnO Oxide Percents 0.75 0.85 0.76 Na2O Oxide Percents 0.36 0.37 0.33 K2O Oxide Percents 0.09 0.02 0.06 BaO Oxide Percents Oxide Totals 99.55 100.26 99.42

213 unit Gardiner River Gardiner River Gardiner River Gardiner River sample GR-3-1 GR-3-1 GR-3-1 GR-3-1 description cpx 1 cpx 1 cpx 1 cpx 1 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 10 G 164 165 166 167

FeO Oxide Percents 7.39 8.07 9.54 8.79 TiO2 Oxide Percents 0.63 0.58 0.86 0.84 CaO Oxide Percents 19.50 18.09 17.05 17.67 SiO2 Oxide Percents 51.88 52.03 50.58 51.74 Al2O3 Oxide Percents 3.22 3.03 3.93 3.51 MgO Oxide Percents 16.54 17.42 17.24 17.24 MnO Oxide Percents 0.16 0.17 0.24 0.21 Na2O Oxide Percents 0.39 0.40 0.40 0.38 K2O Oxide Percents 0.02 0.03 0.00 0.01 BaO Oxide Percents Oxide Totals 99.72 99.81 99.84 100.38

Sc45(LR) 146.60 Ti47(LR) 5496.93 Rb85(LR) 0.00 Sr88(LR) 33.50 Y89(LR) 28.30 Zr90(LR) 34.22 Nb93(LR) 0.11 Cs133(LR) 0.05 Ba138(LR) 0.27 La139(LR) 2.01 Ce140(LR) 5.97 Pr141(LR) 1.34 Nd146(LR) 9.29 Sm147(LR) 3.79 Eu151(LR) 1.28 Gd160(LR) 5.19 Tb159(LR) 0.88 Dy163(LR) 5.54 Ho165(LR) 1.12 Er166(LR) 2.76 Tm169(LR) 0.35 Yb172(LR) 2.10 Lu175(LR) 0.37 Hf178(LR) 1.78 Ta181(LR) 0.04 Pb208(LR) 0.68 Th232(LR) 0.06 U238(LR) 0.01

214 unit Gardiner River Gardiner River Gardiner River Gardiner River sample GR-3-1 GR-3-1 GR-3-1 GR-3-1 description cpx 2 cpx 2 cpx 4 cpx 4 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 11 G 168 170 217 218

FeO Oxide Percents 8.15 9.20 26.73 27.20 TiO2 Oxide Percents 0.72 1.05 0.22 0.21 CaO Oxide Percents 18.99 17.53 18.87 18.99 SiO2 Oxide Percents 51.22 50.66 47.56 47.68 Al2O3 Oxide Percents 3.08 3.95 0.63 0.57 MgO Oxide Percents 16.35 16.64 2.85 2.49 MnO Oxide Percents 0.19 0.23 0.89 0.76 Na2O Oxide Percents 0.35 0.31 0.38 0.41 K2O Oxide Percents -0.02 0.01 0.07 0.07 BaO Oxide Percents Oxide Totals 99.03 99.56 98.19 98.38

Sc45(LR) 110.07 168.38 191.46 Ti47(LR) 4537.10 1153.08 1400.14 Rb85(LR) 0.96 0.03 0.00 Sr88(LR) 32.02 12.49 19.26 Y89(LR) 30.43 202.40 204.90 Zr90(LR) 35.85 60.20 73.73 Nb93(LR) 0.77 0.20 0.24 Cs133(LR) -0.01 0.00 0.00 Ba138(LR) 5.59 0.70 1.11 La139(LR) 4.64 51.53 51.64 Ce140(LR) 11.00 181.50 181.79 Pr141(LR) 1.98 33.30 33.01 Nd146(LR) 11.11 178.94 176.74 Sm147(LR) 4.16 52.76 53.47 Eu151(LR) 0.93 3.15 4.06 Gd160(LR) 4.66 49.28 48.87 Tb159(LR) 0.87 8.29 8.30 Dy163(LR) 5.43 46.69 47.32 Ho165(LR) 1.10 8.69 8.77 Er166(LR) 2.99 21.66 22.00 Tm169(LR) 0.39 3.06 3.10 Yb172(LR) 2.40 20.62 20.04 Lu175(LR) 0.35 4.41 4.17 Hf178(LR) 1.80 2.87 3.35 Ta181(LR) 0.04 0.02 0.01 Pb208(LR) 2.78 1.21 1.32 Th232(LR) 0.57 0.06 0.08 U238(LR) 0.08 0.02 0.02

215 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description rrr date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 95 699 700 702

FeO Oxide Percents 19.18 18.14 18.17 TiO2 Oxide Percents 0.20 0.28 0.28 CaO Oxide Percents 18.12 18.30 17.91 SiO2 Oxide Percents 50.37 51.23 50.97 Al2O3 Oxide Percents 0.73 0.65 0.69 MgO Oxide Percents 9.74 10.32 10.68 MnO Oxide Percents 0.58 0.52 0.61 Na2O Oxide Percents 0.30 0.41 0.28 K2O Oxide Percents 0.07 -0.01 0.02 BaO Oxide Percents Oxide Totals 99.28 99.84 99.61

216 unit Gardiner River Gardiner River sample GR-1 GR-1 description rr date 7/13/2009 7/13/2009 Line Numbers 703 704

FeO Oxide Percents 22.34 19.50 TiO2 Oxide Percents 0.40 0.20 CaO Oxide Percents 20.25 19.05 SiO2 Oxide Percents 49.17 50.94 Al2O3 Oxide Percents 0.77 0.74 MgO Oxide Percents 5.79 8.31 MnO Oxide Percents 0.75 0.49 Na2O Oxide Percents 0.33 0.41 K2O Oxide Percents 0.04 0.08 BaO Oxide Percents Oxide Totals 99.83 99.70

217 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description ccc date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 96 GR 705 706 707

FeO Oxide Percents 27.00 26.45 26.88 TiO2 Oxide Percents 0.20 0.25 0.21 CaO Oxide Percents 19.46 20.21 19.26 SiO2 Oxide Percents 48.51 48.82 48.17 Al2O3 Oxide Percents 0.55 0.52 0.60 MgO Oxide Percents 3.19 3.34 3.26 MnO Oxide Percents 0.91 0.85 0.88 Na2O Oxide Percents 0.26 0.33 0.28 K2O Oxide Percents 0.00 0.03 0.02 BaO Oxide Percents Oxide Totals 100.06 100.81 99.55

218 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description ccc date 7/13/2009 7/13/2009 7/13/2009 Line Numbers 708 709 710

FeO Oxide Percents 27.30 27.45 26.92 TiO2 Oxide Percents 0.19 0.24 0.24 CaO Oxide Percents 19.06 19.14 18.64 SiO2 Oxide Percents 48.42 48.20 48.72 Al2O3 Oxide Percents 0.56 0.44 0.55 MgO Oxide Percents 3.06 2.96 2.91 MnO Oxide Percents 0.79 0.93 0.88 Na2O Oxide Percents 0.25 0.28 0.31 K2O Oxide Percents -0.01 0.02 0.01 BaO Oxide Percents Oxide Totals 99.62 99.66 99.19

219 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description ccc date 7/13/2009 7/13/2009 7/13/2009 Line Numbers 711 712 713

FeO Oxide Percents 27.51 27.19 24.08 TiO2 Oxide Percents 0.20 0.19 0.16 CaO Oxide Percents 19.24 19.11 20.48 SiO2 Oxide Percents 48.53 48.57 48.08 Al2O3 Oxide Percents 0.48 0.48 0.80 MgO Oxide Percents 2.93 2.91 4.65 MnO Oxide Percents 0.84 0.93 0.77 Na2O Oxide Percents 0.26 0.27 0.30 K2O Oxide Percents 0.01 0.01 0.01 BaO Oxide Percents Oxide Totals 99.99 99.68 99.32

Sc45(LR) 142.46 Ti47(LR) 1173.70 Rb85(LR) 0.37 Sr88(LR) 14.81 Y89(LR) 167.46 Zr90(LR) 55.58 Nb93(LR) 0.37 Cs133(LR) 0.00 Ba138(LR) 2.11 La139(LR) 49.61 Ce140(LR) 187.97 Pr141(LR) 31.70 Nd146(LR) 162.46 Sm147(LR) 46.48 Eu151(LR) 3.35 Gd160(LR) 43.46 Tb159(LR) 7.25 Dy163(LR) 40.26 Ho165(LR) 7.36 Er166(LR) 19.37 Tm169(LR) 2.67 Yb172(LR) 18.16 Lu175(LR) 3.74 Hf178(LR) 2.46 Ta181(LR) 0.00 Pb208(LR) 1.19 Th232(LR) 0.21 U238(LR) 0.03

220 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description corona corona corona date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 101 G 735 736 737

FeO Oxide Percents 12.65 8.10 10.76 TiO2 Oxide Percents 0.56 0.50 0.57 CaO Oxide Percents 18.41 17.94 17.60 SiO2 Oxide Percents 51.81 53.13 51.71 Al2O3 Oxide Percents 1.46 1.71 1.85 MgO Oxide Percents 14.14 17.75 15.82 MnO Oxide Percents 0.29 0.20 0.23 Na2O Oxide Percents 0.29 0.32 0.35 K2O Oxide Percents 0.04 0.02 0.07 BaO Oxide Percents Oxide Totals 99.63 99.67 98.94

221 unit Gardiner River Gardiner River sample GR-1 GR-1 description corona corona date 7/13/2009 7/13/2009 Line Numbers 738 739

FeO Oxide Percents 9.10 8.66 TiO2 Oxide Percents 0.49 0.41 CaO Oxide Percents 17.19 17.70 SiO2 Oxide Percents 53.02 53.33 Al2O3 Oxide Percents 1.48 1.42 MgO Oxide Percents 18.37 18.09 MnO Oxide Percents 0.25 0.22 Na2O Oxide Percents 0.27 0.26 K2O Oxide Percents 0.02 0.03 BaO Oxide Percents Oxide Totals 100.19 100.12

222

APPENDIX F

RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF OLIVINE FROM THE MINGLED MAGMAS

unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B GL-4B description ol ol ol ol date 4/29/2009 4/29/2009 4/29/2009 4/29/2009 Line Numbers Un 4 G 130 Un 5 G 131 132 Un 7 G 134 FeO Oxide Percents 19.51 19.78 20.01 18.48 TiO2 Oxide Percents 0.01 0.02 0.00 0.00 CaO Oxide Percents 0.24 0.28 0.25 0.26 SiO2 Oxide Percents 39.56 39.09 39.13 39.57 Al2O3 Oxide Percents 0.01 0.09 0.08 0.05 MgO Oxide Percents 41.53 40.78 40.39 42.17 MnO Oxide Percents 0.27 0.24 0.28 0.28 Na2O Oxide Percents 0.00 0.01 0.01 0.03 K2O Oxide Percents 0.00 0.00 0.00 0.01 Oxide Totals 101.08 100.28 100.14 100.86

224 unit Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B description ol ol ol date 4/29/2009 4/29/2009 4/29/2009 Line Numbers Un 8 G 135 Un 9 G 136 Un 11 G 138 FeO Oxide Percents 18.03 20.04 18.90 TiO2 Oxide Percents 0.00 0.00 0.00 CaO Oxide Percents 0.22 0.27 0.32 SiO2 Oxide Percents 39.46 39.29 39.28 Al2O3 Oxide Percents 0.01 0.06 0.01 MgO Oxide Percents 42.60 41.04 42.18 MnO Oxide Percents 0.24 0.26 0.28 Na2O Oxide Percents 0.00 0.01 0.00 K2O Oxide Percents 0.00 0.04 0.00 Oxide Totals 100.57 101.02 100.98

225 unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B GL-4B description ol ol ol ol date 4/29/2009 4/29/2009 4/29/2009 4/29/2009 Line Numbers Un 17 G 145 Un 21 G 151 Un 29 G 173 174 FeO Oxide Percents 18.91 18.26 19.61 19.75 TiO2 Oxide Percents 0.00 0.00 0.06 0.00 CaO Oxide Percents 0.23 0.22 0.28 0.23 SiO2 Oxide Percents 39.28 39.63 39.76 39.12 Al2O3 Oxide Percents 0.00 0.05 0.05 0.04 MgO Oxide Percents 41.74 42.12 41.17 41.37 MnO Oxide Percents 0.29 0.23 0.23 0.25 Na2O Oxide Percents 0.00 0.00 0.03 0.00 K2O Oxide Percents 0.00 0.01 0.01 0.00 Oxide Totals 100.46 100.52 101.19 100.77

226 unit Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-5B GL-5B description ol ol ol? date 4/29/2009 7/13/2009 7/13/2009 Line Numbers Un 32 G 183 Un 13 G 175 Un 59 G 487 FeO Oxide Percents 21.55 19.07 66.42 TiO2 Oxide Percents 0.02 0.01 0.00 CaO Oxide Percents 0.32 0.30 0.20 SiO2 Oxide Percents 38.69 38.18 30.10 Al2O3 Oxide Percents 0.13 0.04 0.00 MgO Oxide Percents 39.70 41.41 1.57 MnO Oxide Percents 0.28 0.28 2.06 Na2O Oxide Percents 0.03 0.00 0.00 K2O Oxide Percents 0.02 0.02 0.00 Oxide Totals 100.75 99.31 100.35

227 unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-5B GL-5B GL-5B GL-5B GL-5B description ol ol ol ol ol date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 64 G 502 503 504 505 506 FeO Oxide Percents 16.98 16.89 18.31 18.68 19.13 TiO2 Oxide Percents 0.00 0.00 0.04 0.00 0.02 CaO Oxide Percents 0.24 0.28 0.26 0.26 0.25 SiO2 Oxide Percents 39.46 39.28 38.98 38.94 39.25 Al2O3 Oxide Percents 0.05 0.03 0.01 0.02 0.08 MgO Oxide Percents 43.71 43.68 42.26 41.95 41.86 MnO Oxide Percents 0.25 0.19 0.32 0.25 0.24 Na2O Oxide Percents 0.00 0.00 0.01 0.00 0.00 K2O Oxide Percents 0.00 0.02 0.02 0.00 0.00 Oxide Totals 100.68 100.36 100.22 100.10 100.83

228 unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-5B GL-5B GL-5B GL-5B GL-5B description ol ol ol ol ol date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 507 508 509 510 511 FeO Oxide Percents 18.55 17.90 16.76 18.89 22.59 TiO2 Oxide Percents 0.02 0.00 0.01 0.02 0.00 CaO Oxide Percents 0.27 0.28 0.23 0.23 0.27 SiO2 Oxide Percents 39.13 39.43 39.59 38.95 38.68 Al2O3 Oxide Percents 0.06 0.03 0.04 0.06 0.19 MgO Oxide Percents 42.39 43.04 43.74 42.05 38.48 MnO Oxide Percents 0.26 0.22 0.27 0.24 0.38 Na2O Oxide Percents 0.00 0.02 0.01 0.02 0.06 K2O Oxide Percents 0.00 0.00 0.01 0.00 0.04 Oxide Totals 100.66 100.92 100.66 100.46 100.68

229 unit Grizzly Lake Grizzly Lake sample GL-5B GL-5B description ol ol date 7/13/2009 7/13/2009 Line Numbers Un 70 G 529 530 FeO Oxide Percents 19.31 18.92 TiO2 Oxide Percents 0.00 0.01 CaO Oxide Percents 0.31 0.27 SiO2 Oxide Percents 38.96 39.01 Al2O3 Oxide Percents 0.04 0.02 MgO Oxide Percents 41.22 41.95 MnO Oxide Percents 0.30 0.29 Na2O Oxide Percents 0.00 0.03 K2O Oxide Percents 0.02 0.01 Oxide Totals 100.15 100.51

230 unit Grizzly Lake Grizzly Lake Grizzly Lake sample GL-5B GL-5B GL-5B description ol ol ol date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 72 GL 535 536 537 FeO Oxide Percents 19.44 19.83 20.08 TiO2 Oxide Percents 0.00 0.00 0.03 CaO Oxide Percents 0.27 0.27 0.28 SiO2 Oxide Percents 38.68 38.89 38.84 Al2O3 Oxide Percents 0.02 0.06 0.07 MgO Oxide Percents 41.15 41.16 40.72 MnO Oxide Percents 0.32 0.26 0.28 Na2O Oxide Percents 0.02 0.03 0.02 K2O Oxide Percents 0.01 0.01 0.03 Oxide Totals 99.91 100.50 100.35

231 unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C 08CP69C description ol ol ol ol date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers Un 37 08C 319 320 321 322 FeO Oxide Percents 17.35 17.23 18.16 16.87 TiO2 Oxide Percents 0.00 0.04 0.00 0.00 CaO Oxide Percents 0.31 0.31 0.30 0.36 SiO2 Oxide Percents 39.18 38.54 39.15 39.64 Al2O3 Oxide Percents 0.17 0.16 0.12 0.17 MgO Oxide Percents 43.05 42.79 42.30 43.73 MnO Oxide Percents 0.23 0.18 0.24 0.27 Na2O Oxide Percents 0.03 0.03 0.00 0.04 K2O Oxide Percents 0.02 0.01 0.02 0.04 Oxide Totals 100.34 99.30 100.30 101.12

232 unit Crystal Springs Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C 08CP69C description ol ol ol ol date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 323 324 325 326 FeO Oxide Percents 18.33 18.61 17.35 17.34 TiO2 Oxide Percents 0.00 0.00 0.00 0.00 CaO Oxide Percents 0.43 0.41 0.32 0.34 SiO2 Oxide Percents 38.68 38.77 39.42 39.26 Al2O3 Oxide Percents 0.31 0.39 0.17 0.19 MgO Oxide Percents 43.01 41.69 43.37 43.37 MnO Oxide Percents 0.30 0.28 0.27 0.20 Na2O Oxide Percents 0.05 0.07 0.00 0.04 K2O Oxide Percents 0.00 0.00 0.00 0.01 Oxide Totals 101.10 100.21 100.90 100.75

233

APPENDIX G

RESOURCES FOR CHAPTER 2 – MICROPROBE ANALYSES OF GROUNDMASS FROM THE MINGLED MAGMAS

unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B GL-4B description dk bk gls dk bk gls dk bk gls dk bk gls date 4/29/2009 4/29/2009 4/29/2009 4/29/2009 Line Numbers Un 22 G 152 153 155 156

TiO2 Oxide Percents 0.22 0.21 0.17 6.38 MgO Oxide Percents 0.25 0.31 0.04 2.30 MnO Oxide Percents 0.03 0.01 0.01 0.22 CaO Oxide Percents 6.17 2.67 2.87 2.33 K2O Oxide Percents 0.90 1.87 3.03 1.41 SiO2 Oxide Percents 63.98 75.08 73.67 58.99 Al2O3 Oxide Percents 20.52 12.13 14.85 7.80 FeO Oxide Percents 1.28 3.99 0.54 18.43 Na2O Oxide Percents 5.66 2.88 4.20 2.35 Oxide Totals 99.00 99.15 99.38 100.20

235 unit Grizzly Lake Grizzly Lake sample GL-4B GL-4B description dk gy gls dk gy gls date 4/29/2009 4/29/2009 Line Numbers Un 23 G 157 158

TiO2 Oxide Percents 0.13 0.23 MgO Oxide Percents 0.01 3.30 MnO Oxide Percents 0.06 0.13 CaO Oxide Percents 0.50 5.17 K2O Oxide Percents 7.80 2.50 SiO2 Oxide Percents 72.63 59.33 Al2O3 Oxide Percents 13.20 14.30 FeO Oxide Percents 0.64 7.09 Na2O Oxide Percents 2.71 4.05 Oxide Totals 97.68 96.10

236 unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B GL-4B description red gls red gls red gls red gls date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 32 GL 270 271 272 273

TiO2 Oxide Percents 0.85 0.68 0.10 0.97 MgO Oxide Percents 14.86 11.86 0.37 6.60 MnO Oxide Percents 0.31 0.31 0.07 0.21 CaO Oxide Percents 14.50 13.32 10.48 9.84 K2O Oxide Percents 0.26 0.62 0.48 1.33 SiO2 Oxide Percents 50.31 51.45 52.43 52.03 Al2O3 Oxide Percents 4.43 6.28 26.14 11.47 FeO Oxide Percents 10.57 10.31 1.54 7.21 Na2O Oxide Percents 0.89 1.59 5.29 3.45 Oxide Totals 96.98 96.42 96.91 93.09

237 unit Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B description blk gls gry gls gry gls date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 33 G 275 Un 34 GL 278 279

TiO2 Oxide Percents 0.60 1.28 0.92 MgO Oxide Percents 0.72 10.41 9.38 MnO Oxide Percents 0.20 0.14 0.19 CaO Oxide Percents 5.13 13.18 12.25 K2O Oxide Percents 2.64 1.23 1.62 SiO2 Oxide Percents 59.52 53.64 51.99 Al2O3 Oxide Percents 18.02 6.69 8.59 FeO Oxide Percents 3.71 8.95 8.89 Na2O Oxide Percents 4.86 1.42 1.95 Oxide Totals 95.40 96.92 95.76

238 unit Grizzly Lake Grizzly Lake Grizzly Lake Grizzly Lake sample GL-4B GL-4B GL-4B GL-4B description gry gls gry gls mat 2 mat 2 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 280 281 Un 35 GL 282 283

TiO2 Oxide Percents 0.20 0.51 0.98 0.61 MgO Oxide Percents 0.30 0.75 10.95 12.29 MnO Oxide Percents 0.01 0.05 0.22 0.33 CaO Oxide Percents 10.26 4.79 13.73 16.05 K2O Oxide Percents 1.45 3.15 1.22 0.29 SiO2 Oxide Percents 54.88 62.10 51.55 50.73 Al2O3 Oxide Percents 25.43 17.16 5.92 2.76 FeO Oxide Percents 1.34 3.50 10.78 11.82 Na2O Oxide Percents 4.28 4.70 1.24 0.61 Oxide Totals 98.15 96.71 96.60 95.49

239 unit Grizzly Lake Grizzly Lake sample GL-4B GL-4B description mat 2 mat 2 date 7/13/2009 7/13/2009 Line Numbers 284 285

TiO2 Oxide Percents 0.64 0.64 MgO Oxide Percents 13.32 0.78 MnO Oxide Percents 0.42 0.04 CaO Oxide Percents 16.62 6.46 K2O Oxide Percents 0.18 2.30 SiO2 Oxide Percents 50.75 58.86 Al2O3 Oxide Percents 2.49 19.43 FeO Oxide Percents 10.78 3.09 Na2O Oxide Percents 0.41 4.98 Oxide Totals 95.59 96.58

240 unit Gardiner River Gardiner River sample GR-1 GR-1 description glass 1 glass 1 date 7/13/2009 7/13/2009 Line Numbers Un 103 G 744 745

TiO2 Oxide Percents 0.19 0.07 MgO Oxide Percents 0.00 0.00 MnO Oxide Percents 0.02 0.02 CaO Oxide Percents 0.37 0.57 K2O Oxide Percents 5.97 4.60 SiO2 Oxide Percents 77.01 77.00 Al2O3 Oxide Percents 12.82 13.19 FeO Oxide Percents 0.47 0.27 Na2O Oxide Percents 3.70 4.29 Oxide Totals 100.52 100.00

241 unit Gardiner River Gardiner River sample GR-1 GR-1 description glass 1 glass 1 date 7/13/2009 7/13/2009 Line Numbers 746 747

TiO2 Oxide Percents 0.16 0.03 MgO Oxide Percents 0.02 0.00 MnO Oxide Percents 0.02 0.04 CaO Oxide Percents 0.22 5.89 K2O Oxide Percents 6.63 0.79 SiO2 Oxide Percents 75.94 60.56 Al2O3 Oxide Percents 13.18 24.14 FeO Oxide Percents 0.36 0.56 Na2O Oxide Percents 3.37 7.70 Oxide Totals 99.90 99.71

Sc45(LR) 5.82 Ti47(LR) 1585.40 Rb85(LR) 219.59 Sr88(LR) 45.97 Y89(LR) 47.40 Zr90(LR) 194.32 Nb93(LR) 43.29 Cs133(LR) 0.88 Ba138(LR) 739.45 La139(LR) 45.61 Ce140(LR) 83.80 Pr141(LR) 8.47 Nd146(LR) 34.69 Sm147(LR) 7.79 Eu151(LR) 0.94 Gd160(LR) 7.77 Tb159(LR) 1.44 Dy163(LR) 8.23 Ho165(LR) 1.84 Er166(LR) 4.90 Tm169(LR) 0.68 Yb172(LR) 4.25 Lu175(LR) 0.70 Hf178(LR) 7.49 Ta181(LR) 2.60 Pb208(LR) 28.81 Th232(LR) 18.83 U238(LR) 6.80

242 unit Gardiner River Gardiner River sample GR-1 GR-1 description dk gy gls 1 dk gy gls 1 date 7/13/2009 7/13/2009 Line Numbers Un 105 GR 751 752

TiO2 Oxide Percents 1.00 1.18 MgO Oxide Percents 14.04 14.23 MnO Oxide Percents 0.41 0.29 CaO Oxide Percents 16.56 17.31 K2O Oxide Percents 0.07 0.05 SiO2 Oxide Percents 49.83 50.23 Al2O3 Oxide Percents 3.21 3.63 FeO Oxide Percents 14.07 12.51 Na2O Oxide Percents 0.34 0.29 Oxide Totals 99.55 99.72

Sc45(LR) 17.55 Ti47(LR) 5742.75 Rb85(LR) 27.51 Sr88(LR) 91.36 Y89(LR) 41.10 Zr90(LR) 140.22 Nb93(LR) 26.32 Cs133(LR) 1.07 Ba138(LR) 232.95 La139(LR) 38.69 Ce140(LR) 80.20 Pr141(LR) 8.66 Nd146(LR) 34.72 Sm147(LR) 8.26 Eu151(LR) 1.21 Gd160(LR) 7.38 Tb159(LR) 1.33 Dy163(LR) 7.78 Ho165(LR) 1.55 Er166(LR) 4.25 Tm169(LR) 0.60 Yb172(LR) 3.64 Lu175(LR) 0.56 Hf178(LR) 4.70 Ta181(LR) 1.43 Pb208(LR) 17.01 Th232(LR) 10.37 U238(LR) 3.06

243 unit Gardiner River Gardiner River sample GR-1 GR-1 description dk gy gls 1 dk gy gls 1 date 7/13/2009 7/13/2009 Line Numbers 753 754

TiO2 Oxide Percents 0.92 0.82 MgO Oxide Percents 15.50 16.69 MnO Oxide Percents 0.32 0.23 CaO Oxide Percents 16.41 17.62 K2O Oxide Percents 0.04 0.00 SiO2 Oxide Percents 50.45 51.53 Al2O3 Oxide Percents 3.58 3.72 FeO Oxide Percents 11.72 8.90 Na2O Oxide Percents 0.35 0.30 Oxide Totals 99.28 99.79

Sc45(LR) 18.77 Ti47(LR) 7092.68 Rb85(LR) 28.56 Sr88(LR) 89.67 Y89(LR) 38.91 Zr90(LR) 160.00 Nb93(LR) 25.59 Cs133(LR) 1.12 Ba138(LR) 196.22 La139(LR) 34.68 Ce140(LR) 72.58 Pr141(LR) 8.21 Nd146(LR) 31.87 Sm147(LR) 7.08 Eu151(LR) 1.05 Gd160(LR) 6.54 Tb159(LR) 1.14 Dy163(LR) 6.70 Ho165(LR) 1.34 Er166(LR) 3.53 Tm169(LR) 0.50 Yb172(LR) 3.14 Lu175(LR) 0.50 Hf178(LR) 5.25 Ta181(LR) 1.44 Pb208(LR) 17.70 Th232(LR) 12.16 U238(LR) 3.58

244 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description glass 2 glass 2 glass 2 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 106 G 755 756 757

TiO2 Oxide Percents 0.20 0.18 0.13 MgO Oxide Percents 0.01 0.00 0.00 MnO Oxide Percents 0.03 0.00 0.01 CaO Oxide Percents 0.30 0.38 0.31 K2O Oxide Percents 5.86 5.68 6.37 SiO2 Oxide Percents 76.56 77.00 76.98 Al2O3 Oxide Percents 12.79 13.06 12.80 FeO Oxide Percents 0.42 0.40 0.38 Na2O Oxide Percents 3.44 3.64 3.34 Oxide Totals 99.62 100.29 100.31

245 unit Gardiner River Gardiner River Gardiner River sample GR-1 GR-1 GR-1 description glass 2 glass 2 glass 2 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers 758 759 760

TiO2 Oxide Percents 0.11 0.13 0.10 MgO Oxide Percents 0.00 0.00 0.01 MnO Oxide Percents 0.01 0.00 0.00 CaO Oxide Percents 0.33 0.60 0.64 K2O Oxide Percents 5.70 4.75 4.23 SiO2 Oxide Percents 77.23 76.68 77.76 Al2O3 Oxide Percents 12.58 12.88 12.80 FeO Oxide Percents 0.31 0.38 0.35 Na2O Oxide Percents 3.49 4.03 4.37 Oxide Totals 99.77 99.40 100.22

Sc45(LR) 5.44 6.57 Ti47(LR) 1287.87 1407.23 Rb85(LR) 157.95 239.08 Sr88(LR) 32.65 10.71 Y89(LR) 42.89 75.41 Zr90(LR) 155.65 171.64 Nb93(LR) 32.77 39.85 Cs133(LR) 0.64 1.61 Ba138(LR) 569.45 140.54 La139(LR) 42.51 62.75 Ce140(LR) 78.49 114.78 Pr141(LR) 8.26 12.20 Nd146(LR) 34.70 49.61 Sm147(LR) 7.96 11.87 Eu151(LR) 0.76 0.40 Gd160(LR) 8.09 11.37 Tb159(LR) 1.43 2.08 Dy163(LR) 8.61 12.05 Ho165(LR) 1.72 2.36 Er166(LR) 4.64 6.29 Tm169(LR) 0.66 0.86 Yb172(LR) 3.75 5.08 Lu175(LR) 0.58 0.79 Hf178(LR) 6.56 6.17 Ta181(LR) 2.28 2.45 Pb208(LR) 26.04 36.18 Th232(LR) 17.43 24.64 U238(LR) 4.79 7.25

246 unit Gardiner River Gardiner River Gardiner River sample GR-3-1B GR-3-1B GR-3-1B description mat 1 mat 1 mat 1 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 9 G 161 162 163

TiO2 Oxide Percents 0.80 0.39 1.78 MgO Oxide Percents 10.70 17.06 15.07 MnO Oxide Percents 0.35 0.45 0.23 CaO Oxide Percents 14.53 8.34 17.23 K2O Oxide Percents 0.21 0.10 0.10 SiO2 Oxide Percents 52.10 52.04 49.21 Al2O3 Oxide Percents 5.44 1.65 5.17 FeO Oxide Percents 15.42 19.16 10.74 Na2O Oxide Percents 1.05 0.20 0.42 Oxide Totals 100.60 99.37 99.94

Sc45(LR) 11.20 Ti47(LR) 5283.38 Rb85(LR) 72.46 Sr88(LR) 115.66 Y89(LR) 37.84 Zr90(LR) 141.17 Nb93(LR) 29.38 Cs133(LR) 1.07 Ba138(LR) 235.03 La139(LR) 38.74 Ce140(LR) 71.90 Pr141(LR) 8.47 Nd146(LR) 36.54 Sm147(LR) 8.16 Eu151(LR) 0.92 Gd160(LR) 5.21 Tb159(LR) 0.93 Dy163(LR) 5.29 Ho165(LR) 0.96 Er166(LR) 2.36 Tm169(LR) 0.35 Yb172(LR) 1.61 Lu175(LR) 0.34 Hf178(LR) 4.15 Ta181(LR) 1.21 Pb208(LR) 15.87 Th232(LR) 11.70 U238(LR) 2.65

247 unit Gardiner River Gardiner River Gardiner River sample GR-3-1B GR-3-1B GR-3-1B description mat 2 mat 2 mat 2 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 12 GR 171 172 173

TiO2 Oxide Percents 0.08 0.96 0.71 MgO Oxide Percents 0.07 15.22 13.81 MnO Oxide Percents 0.00 0.31 0.32 CaO Oxide Percents 9.94 15.10 14.18 K2O Oxide Percents 0.47 0.10 0.10 SiO2 Oxide Percents 55.59 50.79 50.44 Al2O3 Oxide Percents 26.72 3.13 2.41 FeO Oxide Percents 1.27 13.68 16.13 Na2O Oxide Percents 6.41 0.44 0.40 Oxide Totals 100.53 99.74 98.50

Sc45(LR) 4.86 Ti47(LR) 2335.13 Rb85(LR) 210.98 Sr88(LR) 71.11 Y89(LR) 22.81 Zr90(LR) 102.44 Nb93(LR) 19.93 Cs133(LR) 4.55 Ba138(LR) 163.10 La139(LR) 30.99 Ce140(LR) 57.20 Pr141(LR) 6.52 Nd146(LR) 25.29 Sm147(LR) 5.32 Eu151(LR) 0.54 Gd160(LR) 4.78 Tb159(LR) 0.80 Dy163(LR) 4.24 Ho165(LR) 0.95 Er166(LR) 2.44 Tm169(LR) 0.39 Yb172(LR) 3.02 Lu175(LR) 0.49 Hf178(LR) 5.50 Ta181(LR) 1.67 Pb208(LR) 34.16 Th232(LR) 10.80 U238(LR) 2.75

248 unit Gardiner River Gardiner River Gardiner River sample GR-3-1B GR-3-1B GR-3-1B description mat 3 mat 3 mat 3 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 14 G 178 179 180

TiO2 Oxide Percents 1.51 0.75 1.16 MgO Oxide Percents 14.83 15.71 15.32 MnO Oxide Percents 0.28 0.32 0.24 CaO Oxide Percents 15.66 16.34 17.33 K2O Oxide Percents 0.08 0.08 0.05 SiO2 Oxide Percents 48.39 51.20 49.97 Al2O3 Oxide Percents 5.50 2.78 4.12 FeO Oxide Percents 12.28 11.55 10.60 Na2O Oxide Percents 0.48 0.44 0.37 Oxide Totals 98.99 99.17 99.16

Sc45(LR) 16.09 Ti47(LR) 7435.87 Rb85(LR) 61.70 Sr88(LR) 123.41 Y89(LR) 49.02 Zr90(LR) 132.22 Nb93(LR) 41.07 Cs133(LR) 2.15 Ba138(LR) 197.98 La139(LR) 52.02 Ce140(LR) 94.19 Pr141(LR) 10.87 Nd146(LR) 42.65 Sm147(LR) 9.90 Eu151(LR) 1.04 Gd160(LR) 7.50 Tb159(LR) 1.47 Dy163(LR) 7.08 Ho165(LR) 1.53 Er166(LR) 4.51 Tm169(LR) 0.59 Yb172(LR) 3.52 Lu175(LR) 0.60 Hf178(LR) 5.69 Ta181(LR) 2.49 Pb208(LR) 28.29 Th232(LR) 9.62 U238(LR) 1.70

249 unit Gardiner River Gardiner River Gardiner River sample GR-3-1B GR-3-1B GR-3-1B description mat 4 mat 4 mat 4 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 16 G 189 190 191

TiO2 Oxide Percents 1.16 1.06 1.11 MgO Oxide Percents 11.39 11.74 15.87 MnO Oxide Percents 0.41 0.29 0.36 CaO Oxide Percents 16.99 14.94 13.19 K2O Oxide Percents 0.10 0.48 0.17 SiO2 Oxide Percents 48.51 50.16 49.92 Al2O3 Oxide Percents 3.11 4.50 3.56 FeO Oxide Percents 15.84 12.99 13.72 Na2O Oxide Percents 0.44 1.01 0.60 Oxide Totals 97.96 97.19 98.49

250 unit Gardiner River Gardiner River Gardiner River sample GR-3-1B GR-3-1B GR-3-1B description mat 4 mat 4 mat 4 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers 192 193 194

TiO2 Oxide Percents 0.71 0.75 0.22 MgO Oxide Percents 14.56 16.16 14.20 MnO Oxide Percents 0.28 0.25 0.44 CaO Oxide Percents 16.31 16.41 18.20 K2O Oxide Percents 0.05 0.12 0.10 SiO2 Oxide Percents 50.41 51.24 52.59 Al2O3 Oxide Percents 2.61 3.02 1.23 FeO Oxide Percents 13.48 10.68 12.45 Na2O Oxide Percents 0.37 0.43 0.41 Oxide Totals 98.78 99.07 99.84

Sc45(LR) 7.47 Ti47(LR) 3669.13 Rb85(LR) 173.56 Sr88(LR) 67.40 Y89(LR) 41.95 Zr90(LR) 222.60 Nb93(LR) 34.00 Cs133(LR) 5.39 Ba138(LR) 177.00 La139(LR) 40.65 Ce140(LR) 85.65 Pr141(LR) 9.43 Nd146(LR) 36.75 Sm147(LR) 7.97 Eu151(LR) 0.60 Gd160(LR) 7.35 Tb159(LR) 1.30 Dy163(LR) 8.73 Ho165(LR) 1.94 Er166(LR) 5.75 Tm169(LR) 0.81 Yb172(LR) 5.09 Lu175(LR) 0.72 Hf178(LR) 7.28 Ta181(LR) 2.65 Pb208(LR) 30.68 Th232(LR) 21.73 U238(LR) 5.63

251 unit Gardiner River Gardiner River sample GR-3-1B GR-3-1B description mat 5 mat 5 date 7/13/2009 7/13/2009 Line Numbers Un 18 G 195 196

TiO2 Oxide Percents 1.06 1.23 MgO Oxide Percents 11.51 10.58 MnO Oxide Percents 0.17 0.18 CaO Oxide Percents 15.49 13.52 K2O Oxide Percents 0.35 0.81 SiO2 Oxide Percents 50.82 53.18 Al2O3 Oxide Percents 8.55 8.08 FeO Oxide Percents 8.37 8.34 Na2O Oxide Percents 1.66 1.90 Oxide Totals 97.97 97.82

252 unit Gardiner River Gardiner River sample GR-3-1B GR-3-1B description mat 5 mat 5 date 7/13/2009 7/13/2009 Line Numbers 197 198

TiO2 Oxide Percents 0.99 1.20 MgO Oxide Percents 10.04 5.21 MnO Oxide Percents 0.27 0.14 CaO Oxide Percents 12.57 8.39 K2O Oxide Percents 1.02 1.80 SiO2 Oxide Percents 52.26 58.05 Al2O3 Oxide Percents 6.71 10.60 FeO Oxide Percents 11.86 9.01 Na2O Oxide Percents 1.85 3.17 Oxide Totals 97.58 97.56

Sc45(LR) 15.69 Ti47(LR) 7923.53 Rb85(LR) 53.20 Sr88(LR) 141.63 Y89(LR) 36.63 Zr90(LR) 156.88 Nb93(LR) 30.62 Cs133(LR) 1.45 Ba138(LR) 229.90 La139(LR) 33.93 Ce140(LR) 72.48 Pr141(LR) 8.31 Nd146(LR) 32.62 Sm147(LR) 7.45 Eu151(LR) 1.06 Gd160(LR) 6.62 Tb159(LR) 1.19 Dy163(LR) 6.81 Ho165(LR) 1.30 Er166(LR) 3.71 Tm169(LR) 0.49 Yb172(LR) 3.22 Lu175(LR) 0.48 Hf178(LR) 5.16 Ta181(LR) 1.75 Pb208(LR) 23.12 Th232(LR) 11.21 U238(LR) 3.45

253 unit Gardiner River Gardiner River Gardiner River sample GR-3-1B GR-3-1B GR-3-1B description mat 6 mat 6 mat 6 date 7/13/2009 7/13/2009 7/13/2009 Line Numbers Un 21 G 219 220 221

TiO2 Oxide Percents 0.05 0.06 0.04 MgO Oxide Percents 1.20 0.23 0.20 MnO Oxide Percents 0.02 0.00 0.00 CaO Oxide Percents 1.48 0.53 1.10 K2O Oxide Percents 5.63 7.66 7.48 SiO2 Oxide Percents 60.97 69.87 66.42 Al2O3 Oxide Percents 14.66 14.08 16.00 FeO Oxide Percents 2.28 0.65 0.72 Na2O Oxide Percents 4.48 3.70 4.83 Oxide Totals 90.77 96.78 96.79

Sc45(LR) 3.97 Ti47(LR) 812.53 Rb85(LR) 379.17 Sr88(LR) 58.06 Y89(LR) 18.69 Zr90(LR) 125.47 Nb93(LR) 21.56 Cs133(LR) 3.64 Ba138(LR) 316.34 La139(LR) 25.16 Ce140(LR) 44.01 Pr141(LR) 3.53 Nd146(LR) 12.29 Sm147(LR) 2.51 Eu151(LR) 0.55 Gd160(LR) 1.96 Tb159(LR) 0.33 Dy163(LR) 2.31 Ho165(LR) 0.45 Er166(LR) 1.35 Tm169(LR) 0.21 Yb172(LR) 1.20 Lu175(LR) 0.19 Hf178(LR) 4.08 Ta181(LR) 1.28 Pb208(LR) 35.34 Th232(LR) 8.83 U238(LR) 2.52

254 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description rhyo glass rhyo glass rhyo glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers Un 34 0 277 278 279

TiO2 Oxide Percents 0.12 0.04 0.08 MgO Oxide Percents 0.00 0.01 0.05 MnO Oxide Percents 0.00 0.00 0.00 CaO Oxide Percents 0.45 0.75 0.46 K2O Oxide Percents 5.24 4.14 5.51 SiO2 Oxide Percents 76.99 75.29 77.18 Al2O3 Oxide Percents 12.57 13.94 12.40 FeO Oxide Percents 0.94 0.73 1.05 Na2O Oxide Percents 3.57 4.89 3.35 Oxide Totals 99.88 99.80 100.08

255 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description rhyo glass rhyo glass rhyo glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers 280 281 282

TiO2 Oxide Percents 0.09 0.09 0.14 MgO Oxide Percents 0.02 0.03 0.01 MnO Oxide Percents 0.03 0.02 0.00 CaO Oxide Percents 0.33 0.60 0.50 K2O Oxide Percents 5.72 4.96 5.47 SiO2 Oxide Percents 76.41 75.98 76.22 Al2O3 Oxide Percents 12.44 13.39 12.83 FeO Oxide Percents 1.01 0.82 0.87 Na2O Oxide Percents 3.10 4.02 3.36 Oxide Totals 99.14 99.90 99.40

256 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description rhyo glass rhyo glass rhyo glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers 283 284 285

TiO2 Oxide Percents 0.16 0.08 0.15 MgO Oxide Percents 0.02 0.02 0.04 MnO Oxide Percents 0.00 0.02 0.01 CaO Oxide Percents 0.38 0.37 0.40 K2O Oxide Percents 6.00 6.04 5.62 SiO2 Oxide Percents 76.03 76.39 76.90 Al2O3 Oxide Percents 12.70 12.49 12.23 FeO Oxide Percents 1.06 1.05 0.91 Na2O Oxide Percents 3.19 3.07 3.15 Oxide Totals 99.54 99.54 99.42

257 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description rhyo glass rhyo glass rhyo glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers 286 287 288

TiO2 Oxide Percents 0.11 0.11 0.09 MgO Oxide Percents 0.03 0.04 0.06 MnO Oxide Percents 0.04 0.00 0.01 CaO Oxide Percents 0.35 0.37 0.33 K2O Oxide Percents 5.92 5.88 5.92 SiO2 Oxide Percents 76.45 76.82 77.15 Al2O3 Oxide Percents 12.52 12.38 12.41 FeO Oxide Percents 1.09 1.10 1.06 Na2O Oxide Percents 3.17 3.26 3.13 Oxide Totals 99.69 99.93 100.18

258 unit Crystal Springs Crystal Springs sample 08CP69C 08CP69C description rhyo glass rhyo glass date 11/9/2009 11/9/2009 Line Numbers 289 290

TiO2 Oxide Percents 0.13 0.11 MgO Oxide Percents 0.02 0.03 MnO Oxide Percents 0.00 0.08 CaO Oxide Percents 0.37 0.42 K2O Oxide Percents 5.51 5.84 SiO2 Oxide Percents 76.61 76.64 Al2O3 Oxide Percents 12.53 12.58 FeO Oxide Percents 0.96 1.14 Na2O Oxide Percents 3.48 3.06 Oxide Totals 99.62 99.89

259 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description rhyo glass rhyo glass rhyo glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers 291 292 293

TiO2 Oxide Percents 0.09 0.08 0.14 MgO Oxide Percents 0.01 0.01 0.03 MnO Oxide Percents 0.00 0.02 0.03 CaO Oxide Percents 0.38 0.62 0.34 K2O Oxide Percents 5.86 4.99 5.89 SiO2 Oxide Percents 77.03 75.87 76.63 Al2O3 Oxide Percents 12.36 13.16 12.43 FeO Oxide Percents 0.95 0.85 1.13 Na2O Oxide Percents 3.31 3.91 3.14 Oxide Totals 99.99 99.52 99.75

260 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description rhyo glass rhyo glass rhyo glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers 294 295 296

TiO2 Oxide Percents 0.11 0.11 0.14 MgO Oxide Percents 0.04 0.02 0.02 MnO Oxide Percents 0.00 0.01 0.03 CaO Oxide Percents 0.55 0.39 0.35 K2O Oxide Percents 5.16 5.69 5.79 SiO2 Oxide Percents 76.30 76.65 75.75 Al2O3 Oxide Percents 13.04 12.46 11.89 FeO Oxide Percents 0.88 0.95 1.25 Na2O Oxide Percents 3.74 3.19 2.75 Oxide Totals 99.81 99.47 97.97

261 unit Crystal Springs Crystal Springs Crystal Springs sample 08CP69C 08CP69C 08CP69C description mix glass mix glass mix glass date 11/9/2009 11/9/2009 11/9/2009 Line Numbers Un 35 08 297 298 299

TiO2 Oxide Percents 0.13 0.05 0.05 MgO Oxide Percents 0.04 0.27 0.31 MnO Oxide Percents 0.03 0.02 0.04 CaO Oxide Percents 0.37 13.37 11.56 K2O Oxide Percents 5.55 0.19 0.29 SiO2 Oxide Percents 75.28 51.50 55.59 Al2O3 Oxide Percents 12.02 30.24 28.19 FeO Oxide Percents 1.76 0.78 0.97 Na2O Oxide Percents 2.82 3.76 4.47 Oxide Totals 98.00 100.18 101.47

262

APPENDIX H

RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF GROUNDMASS GLASS FROM THE EUBM

unit TSC TSC TSC TSC TSC TSC TSC sample 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 description dk gry glass dk gry glass dk gry glass dk gry glass dk gry glass dk gry glass dk gry glass date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 549 551 553 554 555 556 557 TiO2 Oxide % 0.27 0.26 0.53 0.34 0.02 0.41 0.03 MgO Oxide % 0.31 0.00 0.01 0.16 0.00 0.01 0.00 MnO Oxide % 0.07 0.00 0.00 0.07 0.01 0.06 0.00 CaO Oxide % 1.05 0.34 0.31 0.66 0.26 0.26 0.32 K2O Oxide % 4.78 5.33 5.71 4.29 5.60 4.99 5.26 SiO2 Oxide % 75.99 76.68 76.49 76.07 78.39 78.75 78.45 Al2O3 Oxide % 11.14 12.94 12.74 11.66 12.18 11.62 12.20 FeO Oxide % 3.31 0.47 0.77 2.86 0.20 0.47 0.19 Na2O Oxide % 3.08 4.03 3.45 3.88 3.33 3.43 3.59 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.04 100.00 100.00 100.00 100.00 100.03 Total (RAW) 101.70 101.05 100.77 100.78 100.12 99.97 100.72

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

264 unit TSC TSC TSC TSC TSC TSC TSC sample 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 description dk gry glass dk gry glass dk gry glass dk gry glass dk gry glass dk gry glass lght gry gls date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 558 559 560 561 562 563 567 TiO2 Oxide % 0.24 0.25 0.40 0.66 0.35 0.12 0.19 MgO Oxide % 0.10 0.04 0.02 0.04 0.05 0.02 0.11 MnO Oxide % 0.03 0.04 0.02 0.02 0.01 0.05 0.07 CaO Oxide % 0.58 0.33 0.34 0.45 0.37 0.34 0.57 K2O Oxide % 5.72 4.67 5.01 5.12 4.80 4.56 5.26 SiO2 Oxide % 73.27 77.22 78.47 76.80 76.16 78.75 75.85 Al2O3 Oxide % 14.17 12.14 11.74 12.20 12.31 11.98 11.82 FeO Oxide % 1.81 1.65 0.51 1.35 2.27 0.55 3.82 Na2O Oxide % 4.09 3.65 3.48 3.35 3.70 3.64 2.31 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 101.05 100.96 100.62 98.58 101.70 101.35 99.98

LA-ICP-MS (ppm) Si29 15200925.27 14789852.85 Ca43 0.32 0.38 Sc45 8.11 9.39 Ti47 1868.36 1821.77 Rb85 99.76 104.90 Sr88 14.34 17.60 Y89 67.09 61.46 Zr90 197.79 197.93 Nb93 79.14 75.41 Cs133 5.13 5.47 Ba138 431.89 456.38 La139 99.95 96.70 Ce140 216.06 212.92 Pr141 20.21 20.07 Nd146 75.11 75.42 Sm147 14.48 14.75 Eu151 0.87 0.85 Gd157 11.09 11.10 Tb159 2.06 1.95 Dy163 11.99 11.71 Ho165 2.42 2.35 Er166 6.69 6.34 Tm169 0.95 0.88 Yb172 5.77 5.33 Lu175 0.99 0.94 Hf178 5.93 5.92 Ta181 2.96 3.01 Pb208 42.00 40.72 Th232 27.27 27.35 U238 8.90 8.73

265 unit TSC TSC TSC TSC TSC TSC TSC TSC sample 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 description lght gry gls lght gry gls lght gry gls lght gry gls lght gry gls dk gls 2 dk gls 2 dk gls 2 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 568 569 574 576 578 597 598 599 TiO2 Oxide % 0.17 0.22 0.20 0.19 0.19 0.50 0.41 0.90 MgO Oxide % 0.18 0.04 0.03 0.05 0.07 0.00 0.07 0.00 MnO Oxide % 0.02 0.00 0.00 0.03 0.06 0.00 0.04 0.05 CaO Oxide % 0.93 0.34 0.28 0.29 0.31 0.41 0.47 0.33 K2O Oxide % 5.20 5.65 5.64 5.83 5.55 4.49 4.03 4.43 SiO2 Oxide % 77.14 78.70 78.01 77.95 78.15 76.17 73.60 77.05 Al2O3 Oxide % 11.93 12.27 12.09 12.10 12.05 13.43 12.58 12.10 FeO Oxide % 2.05 0.55 1.53 1.31 1.36 0.49 4.07 1.18 Na2O Oxide % 2.38 2.22 2.22 2.24 2.27 4.55 4.72 3.98 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.03 100.00 100.00 Total (RAW) 98.23 98.39 98.01 98.18 98.44 100.71 98.71 100.59

LA-ICP-MS (ppm) Si29 8791259.21 10934787.65 Ca43 0.51 0.44 Sc45 9.96 8.47 Ti47 1601.99 1473.78 Rb85 299.32 290.21 Sr88 23.42 15.35 Y89 58.31 51.99 Zr90 195.05 184.16 Nb93 64.56 62.02 Cs133 6.96 7.37 Ba138 500.58 445.09 La139 82.30 73.44 Ce140 194.13 176.40 Pr141 17.54 15.47 Nd146 66.08 57.84 Sm147 13.24 11.47 Eu151 1.23 0.94 Gd157 9.58 8.42 Tb159 1.74 1.64 Dy163 10.44 9.71 Ho165 2.04 1.95 Er166 5.70 5.24 Tm169 0.80 0.73 Yb172 4.98 4.61 Lu175 0.84 0.73 Hf178 5.59 5.62 Ta181 2.78 2.72 Pb208 47.21 46.04 Th232 20.50 19.21 U238 9.84 9.12

266 unit TSC TSC TSC TSC TSC TSC TSC TSC TSC sample 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 description dk gls 2 dk gls 2 dk gls 2 dk gls 2 dk gls 2 dk gls 2 dk gls 2 dk gls 2 dk gls 2 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 600 601 602 603 604 605 606 607 608 TiO2 Oxide % 0.37 0.10 0.24 0.17 0.29 0.15 0.03 0.22 0.02 MgO Oxide % 0.03 0.03 0.05 0.16 0.35 0.04 0.03 0.32 0.11 MnO Oxide % 0.05 0.02 0.05 0.06 0.12 0.07 0.01 0.08 0.04 CaO Oxide % 0.44 0.37 0.36 0.69 1.20 0.39 0.50 0.84 0.55 K2O Oxide % 5.07 4.77 3.86 3.02 3.46 4.41 4.28 4.19 4.24 SiO2 Oxide % 75.52 77.27 78.09 79.14 76.48 77.04 79.10 76.60 75.53 Al2O3 Oxide % 13.47 12.53 12.21 11.53 11.57 12.46 11.74 11.77 13.74 FeO Oxide % 0.67 0.76 0.82 0.94 2.64 1.16 0.38 2.21 0.87 Na2O Oxide % 4.37 4.16 4.32 4.29 3.89 4.28 3.92 3.77 4.89 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 100.99 100.48 100.53 99.94 100.86 100.21 100.29 100.78 100.30

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

267 unit TSC TSC TSC TSC TSC TSC TSC sample 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 description dk gls 2 dk gls 2 dk gls 2 dk gls 2 lght gry gls 2 lght gry gls 2 lght gry gls 2 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 609 611 613 614 624 632 633 TiO2 Oxide % 0.31 0.03 0.19 0.31 0.23 0.21 0.15 MgO Oxide % 0.00 0.09 0.00 0.08 0.34 0.28 0.17 MnO Oxide % 0.04 0.00 0.05 0.00 0.10 0.08 0.03 CaO Oxide % 0.45 0.39 0.33 0.39 1.40 1.02 0.90 K2O Oxide % 5.04 4.21 4.78 4.29 5.26 5.39 5.55 SiO2 Oxide % 75.34 78.67 76.75 75.59 75.06 77.02 77.60 Al2O3 Oxide % 13.09 12.02 12.55 12.96 11.70 11.93 11.92 FeO Oxide % 1.49 0.68 1.27 1.91 3.60 1.82 1.43 Na2O Oxide % 4.24 3.92 4.10 4.46 2.31 2.26 2.24 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.02 100.00 100.00 100.00 100.00 Total (RAW) 98.56 99.83 99.91 100.44 98.10 98.07 98.48

LA-ICP-MS (ppm) Si29 11518415.72 10532337.96 Ca43 0.27 0.38 Sc45 13.87 10.06 Ti47 2000.46 2095.95 Rb85 389.15 83.77 Sr88 11.97 17.01 Y89 137.28 79.57 Zr90 255.69 237.43 Nb93 83.50 81.64 Cs133 7.50 6.01 Ba138 359.20 464.27 La139 178.82 120.05 Ce140 377.97 231.43 Pr141 44.00 22.92 Nd146 189.42 87.79 Sm147 38.97 17.07 Eu151 3.28 1.03 Gd157 29.30 13.20 Tb159 5.13 2.48 Dy163 31.03 14.43 Ho165 5.84 2.91 Er166 15.07 7.94 Tm169 2.08 1.10 Yb172 14.01 6.58 Lu175 2.12 1.15 Hf178 7.01 6.80 Ta181 3.31 3.41 Pb208 43.80 41.30 Th232 34.99 32.80 U238 9.72 9.06

268 unit TSC TSC TSC TSC TSC TSC TSC TSC TSC sample 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 07CP12 description lght gry gls 2 dk gls 3 dk gls 3 dk gls 3 dk gls 3 dk gls 3 dk gls 3 dk gls 3 dk gls 3 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 634 660 663 665 666 669 670 671 672 TiO2 Oxide % 0.28 0.30 0.23 0.31 0.04 0.27 0.10 0.10 0.07 MgO Oxide % 0.07 0.12 0.39 0.04 0.01 0.06 0.04 0.03 0.00 MnO Oxide % 0.03 0.07 0.12 0.06 0.02 0.01 0.01 0.06 0.02 CaO Oxide % 1.05 0.56 1.56 0.39 0.38 0.41 0.41 0.35 0.32 K2O Oxide % 3.59 4.63 3.42 3.93 4.42 4.01 4.61 4.74 5.27 SiO2 Oxide % 76.33 74.92 78.03 77.03 78.54 78.18 78.24 78.17 76.76 Al2O3 Oxide % 12.29 13.10 10.21 12.16 12.35 11.59 12.01 12.32 13.47 FeO Oxide % 3.30 1.99 2.71 1.86 0.31 1.67 0.71 0.37 0.17 Na2O Oxide % 3.07 4.31 3.34 4.21 3.94 3.80 3.87 3.86 3.94 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.02 Total (RAW) 99.08 100.15 100.19 100.49 100.89 101.25 100.87 100.52 102.07

LA-ICP-MS (ppm) Si29 7014575.65 Ca43 0.56 Sc45 9.94 Ti47 1650.65 Rb85 328.23 Sr88 16.44 Y89 71.10 Zr90 208.48 Nb93 68.45 Cs133 7.31 Ba138 479.85 La139 94.51 Ce140 209.50 Pr141 19.69 Nd146 73.91 Sm147 14.62 Eu151 1.34 Gd157 11.03 Tb159 1.97 Dy163 12.23 Ho165 2.40 Er166 6.45 Tm169 0.88 Yb172 5.57 Lu175 0.90 Hf178 6.16 Ta181 2.85 Pb208 49.68 Th232 22.21 U238 11.11

269 unit TSC TSC TSC TSC CAN CAN CAN sample 07CP12 07CP12 07CP12 07CP12 0934 0934 0934 description dk gls 3 lght gry gls 3 lght gry gls 3 lght gry gls 3 glass 1 glass 1 glass 1 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 674 685 689 692 36 37 38 TiO2 Oxide % 0.02 0.14 0.22 0.15 0.18 0.20 0.21 MgO Oxide % 0.00 0.00 0.00 0.00 0.06 0.08 0.09 MnO Oxide % 0.00 0.03 0.01 0.02 0.06 0.03 0.06 CaO Oxide % 0.36 0.17 0.17 0.14 0.51 0.47 0.56 K2O Oxide % 4.48 5.87 6.00 5.90 5.33 5.30 5.40 SiO2 Oxide % 78.04 79.21 79.15 78.99 77.51 77.50 77.55 Al2O3 Oxide % 12.57 12.09 12.02 12.21 12.09 12.05 11.86 FeO Oxide % 0.17 0.28 0.28 0.50 1.30 1.38 1.38 Na2O Oxide % 4.37 2.21 2.16 2.08 2.95 3.00 2.89 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 101.06 98.06 98.41 98.36 96.73 97.66 97.30

LA-ICP-MS (ppm) Si29 14278885.87 10675681.85 Ca43 0.40 0.46 Sc45 8.95 7.67 Ti47 1794.70 1503.39 Rb85 86.84 297.20 Sr88 17.32 17.30 Y89 68.13 63.99 Zr90 215.14 218.66 Nb93 78.71 64.07 Cs133 5.22 6.94 Ba138 453.76 470.25 La139 90.11 87.12 Ce140 173.48 187.79 Pr141 15.73 17.42 Nd146 58.76 67.03 Sm147 11.86 13.51 Eu151 0.88 1.31 Gd157 9.40 10.33 Tb159 1.83 2.02 Dy163 11.64 11.48 Ho165 2.41 2.38 Er166 6.85 6.54 Tm169 1.00 0.90 Yb172 6.11 5.59 Lu175 1.05 0.92 Hf178 6.05 6.96 Ta181 3.09 2.94 Pb208 39.33 45.88 Th232 27.92 22.97 U238 10.98 8.83

270 unit CAN CAN CAN CAN CAN CAN CAN CAN CAN CAN CAN sample 0934 0934 0934 0934 0934 0934 0934 0934 0934 0934 0934 description glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 39 40 41 42 43 44 45 46 47 48 49 TiO2 Oxide % 0.19 0.19 0.15 0.22 0.20 0.22 0.26 0.21 0.20 0.19 0.22 MgO Oxide % 0.08 0.09 0.07 0.07 0.07 0.09 0.08 0.10 0.07 0.06 0.06 MnO Oxide % 0.06 0.03 0.01 0.08 0.05 0.03 0.07 0.02 0.04 0.05 0.02 CaO Oxide % 0.51 0.48 0.42 0.48 0.47 0.54 0.49 0.57 0.54 0.44 0.45 K2O Oxide % 5.43 5.34 5.41 5.27 5.29 5.36 5.46 5.52 5.43 5.33 5.49 SiO2 Oxide % 77.38 77.72 77.32 77.50 77.71 77.45 77.42 77.43 77.50 78.04 77.41 Al2O3 Oxide % 11.99 11.95 12.06 12.06 11.91 11.92 11.94 11.95 11.84 11.91 12.11 FeO Oxide % 1.35 1.28 1.54 1.35 1.30 1.27 1.34 1.23 1.36 0.97 1.24 Na2O Oxide % 3.01 2.92 3.04 2.95 3.00 3.13 2.95 2.97 3.01 3.02 3.00 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 97.05 97.45 97.51 97.11 97.03 97.51 97.59 98.01 97.47 97.03 97.17

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

271 unit CAN CAN CAN CAN CAN CAN CAN CAN CAN sample 0934 0934 0934 0934 0934 0934 0934 0934 0934 description glass 1 glass 1 glass 1 glass 1 glass 1 glass 1 glass 2 glass 2 glass 2 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 50 51 52 53 54 55 146 147 148 TiO2 Oxide % 0.20 0.19 0.20 0.18 0.18 0.22 0.19 0.21 0.17 MgO Oxide % 0.11 0.10 0.06 0.07 0.11 0.10 0.11 0.07 0.07 MnO Oxide % 0.04 0.07 0.03 0.04 0.10 0.05 0.04 0.04 0.01 CaO Oxide % 0.53 0.49 0.52 0.41 0.46 0.52 0.40 0.41 0.36 K2O Oxide % 5.47 5.36 5.25 5.24 5.24 5.51 5.48 5.26 5.45 SiO2 Oxide % 77.44 77.33 77.55 77.50 77.45 77.38 77.42 77.66 77.65 Al2O3 Oxide % 12.00 12.07 11.97 11.99 12.09 11.87 11.95 11.97 11.99 FeO Oxide % 1.33 1.32 1.37 1.47 1.34 1.33 1.32 1.29 1.33 Na2O Oxide % 2.88 3.07 3.05 3.11 3.03 3.02 3.08 3.09 2.98 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 97.72 97.27 97.60 97.28 97.61 97.48 97.47 97.24 97.03

LA-ICP-MS (ppm) Si29 12686391.50 15493126.01 15800519.46 Ca43 0.27 0.30 0.29 Sc45 10.97 10.97 10.56 Ti47 1465.62 1475.38 1423.24 Rb85 225.22 224.29 221.35 Sr88 16.21 17.29 17.20 Y89 45.00 42.88 43.44 Zr90 204.28 199.74 198.13 Nb93 59.56 59.42 58.33 Cs133 4.75 4.86 4.74 Ba138 531.79 521.53 521.11 La139 60.12 57.76 57.32 Ce140 127.26 126.97 127.33 Pr141 12.22 12.02 11.87 Nd146 46.15 44.40 45.31 Sm147 9.09 8.74 9.02 Eu151 0.83 0.83 0.81 Gd157 8.54 7.98 7.77 Tb159 1.42 1.30 1.34 Dy163 8.45 7.86 7.83 Ho165 1.67 1.58 1.60 Er166 4.81 4.26 4.73 Tm169 0.69 0.62 0.66 Yb172 4.36 4.10 4.12 Lu175 0.72 0.59 0.65 Hf178 6.19 5.92 5.98 Ta181 2.99 2.86 3.07 Pb208 36.80 35.34 35.78 Th232 19.04 18.11 18.79 U238 6.81 6.92 6.87

272 unit CAN CAN CAN CAN CAN CAN CAN CAN CAN CAN sample 0934 0934 0934 0934 0934 0934 0934 0934 0934 0934 description glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 149 150 151 152 153 154 155 156 157 158 TiO2 Oxide % 0.19 0.18 0.21 0.19 0.20 0.19 0.21 0.21 0.23 0.13 MgO Oxide % 0.08 0.08 0.09 0.06 0.09 0.09 0.10 0.11 0.12 0.07 MnO Oxide % 0.03 0.08 0.05 0.04 0.07 0.04 0.04 0.00 0.00 0.01 CaO Oxide % 0.48 0.51 0.49 0.46 0.55 0.44 0.51 0.47 0.42 0.51 K2O Oxide % 5.40 5.26 5.42 5.38 5.40 5.22 5.43 5.28 5.44 5.45 SiO2 Oxide % 77.70 77.56 77.35 77.64 77.33 77.55 77.61 77.51 77.60 77.39 Al2O3 Oxide % 11.84 12.02 12.00 11.96 11.95 12.08 11.88 12.00 12.12 12.00 FeO Oxide % 1.29 1.32 1.33 1.34 1.31 1.28 1.27 1.26 1.12 1.33 Na2O Oxide % 3.00 3.00 3.07 2.92 3.09 3.12 2.94 3.16 2.95 3.10 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 97.47 97.37 97.45 97.60 97.46 97.12 97.19 97.19 96.66 96.72

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

273 unit CAN CAN CAN CAN CAN CAN CAN CAN CAN CAN sample 0934 0934 0934 0934 0934 0934 0934 0934 0934 0934 description glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 glass 2 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 159 160 161 162 163 164 165 166 167 168 TiO2 Oxide % 0.17 0.26 0.21 0.15 0.18 0.22 0.23 0.18 0.21 0.26 MgO Oxide % 0.08 0.06 0.06 0.08 0.09 0.08 0.06 0.07 0.08 0.05 MnO Oxide % 0.03 0.06 0.05 0.01 0.07 0.05 0.02 0.05 0.06 0.04 CaO Oxide % 0.50 0.43 0.47 0.46 0.46 0.48 0.48 0.51 0.53 0.53 K2O Oxide % 5.31 5.37 5.32 5.49 5.29 5.35 5.38 5.28 5.43 5.38 SiO2 Oxide % 77.67 77.43 77.27 77.65 77.41 77.40 77.63 77.54 77.43 77.46 Al2O3 Oxide % 11.87 12.02 12.17 11.90 12.03 12.02 11.82 12.07 11.93 11.83 FeO Oxide % 1.29 1.37 1.40 1.24 1.36 1.33 1.30 1.34 1.32 1.37 Na2O Oxide % 3.07 2.99 3.06 3.02 3.10 3.07 3.08 2.95 3.01 3.07 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 96.95 96.35 96.96 97.12 97.40 97.12 97.30 96.97 97.07 97.41

LA-ICP-MS (ppm) Si29 13738046.06 Ca43 0.29 Sc45 10.20 Ti47 1487.99 Rb85 225.90 Sr88 14.78 Y89 41.05 Zr90 187.36 Nb93 58.62 Cs133 5.06 Ba138 492.37 La139 56.75 Ce140 131.93 Pr141 11.51 Nd146 43.08 Sm147 8.40 Eu151 0.76 Gd157 7.53 Tb159 1.23 Dy163 7.51 Ho165 1.56 Er166 4.30 Tm169 0.62 Yb172 3.83 Lu175 0.60 Hf178 5.40 Ta181 2.74 Pb208 36.93 Th232 17.56 U238 7.22

274 unit CAN CAN- silver CAN- silver CAN- silver CAN- silver CAN- silver sample 0934 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B description glass 2 glass 1 glass 1 glass 1 glass 1 glass 1 date 11/9/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 169 869 870 871 872 873 TiO2 Oxide % 0.24 0.02 0.25 0.02 0.05 0.08 MgO Oxide % 0.07 0.00 0.02 0.00 0.00 0.06 MnO Oxide % 0.04 0.03 0.03 0.00 0.02 0.00 CaO Oxide % 0.55 0.24 0.23 0.31 0.32 0.33 K2O Oxide % 5.41 8.81 7.06 7.44 6.19 6.14 SiO2 Oxide % 77.27 68.04 74.86 72.31 76.53 74.01 Al2O3 Oxide % 12.00 17.81 13.00 15.48 13.09 14.31 FeO Oxide % 1.34 0.23 1.42 0.32 0.23 0.76 Na2O Oxide % 3.08 4.84 3.13 4.14 3.57 4.30 P205 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.01 100.00 100.00 100.00 100.01 Total (RAW) 97.36 99.18 98.29 98.59 99.16 98.68

LA-ICP-MS (ppm) Si29 11752654.18 13313768.07 15652125.19 17445445.31 17908041.81 Ca43 0.26 0.23 0.13 0.16 0.16 Sc45 10.53 7.53 7.69 6.95 6.38 Ti47 1446.88 919.09 1258.60 1027.64 880.20 Rb85 235.47 120.11 146.80 157.14 152.78 Sr88 14.46 12.70 12.84 14.88 11.63 Y89 36.89 32.91 35.74 18.61 14.14 Zr90 169.53 153.92 158.75 146.36 138.14 Nb93 58.38 45.45 40.38 39.88 36.68 Cs133 5.22 2.00 2.81 5.32 5.45 Ba138 467.24 435.77 412.49 381.16 346.59 La139 53.06 71.48 92.40 44.44 34.16 Ce140 129.12 150.38 162.59 84.37 67.19 Pr141 10.86 15.02 19.73 8.24 6.12 Nd146 40.24 57.37 75.49 30.68 21.84 Sm147 7.92 10.09 15.31 6.35 4.17 Eu151 0.71 0.48 0.78 0.52 0.43 Gd157 6.98 8.23 12.70 4.69 3.27 Tb159 1.19 1.33 2.04 0.80 0.55 Dy163 6.83 6.86 11.13 4.52 3.21 Ho165 1.46 1.37 1.98 0.72 0.53 Er166 3.85 3.29 4.82 2.05 1.51 Tm169 0.58 0.47 0.63 0.29 0.25 Yb172 3.64 2.76 3.27 1.54 1.31 Lu175 0.57 0.43 0.45 0.27 0.22 Hf178 5.14 5.32 5.21 4.94 4.62 Ta181 2.69 2.25 2.56 2.48 2.28 Pb208 41.68 44.38 44.22 41.85 39.29 Th232 16.50 22.13 25.66 16.18 14.81 U238 7.50 6.10 5.47 5.23 5.29

275 unit CAN- silver CAN- silver CAN- silver DRF DRF DRF DRF sample 08CP21B 08CP21B 08CP21B 08CP09 08CP09 08CP09 08CP09 description glass 2 glass 2 glass 2 glass 1 glass 1 glass 1 glass 3 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 885 886 888 341 343 350 351 TiO2 Oxide % 0.00 0.00 0.06 0.10 0.10 0.14 0.09 MgO Oxide % 0.00 0.00 0.06 0.07 0.06 0.05 0.08 MnO Oxide % 0.07 0.00 0.07 0.06 0.03 0.04 0.04 CaO Oxide % 0.15 0.22 0.34 0.46 0.49 0.42 0.42 K2O Oxide % 9.09 9.69 8.62 5.53 5.60 5.51 5.44 SiO2 Oxide % 68.11 67.05 67.54 76.54 76.76 76.69 76.75 Al2O3 Oxide % 17.71 18.14 17.37 12.03 12.05 12.18 11.90 FeO Oxide % 0.32 0.24 1.29 1.33 1.02 1.05 1.41 Na2O Oxide % 4.59 4.72 4.64 3.89 3.89 3.92 3.86 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.04 100.06 100.00 100.00 100.00 100.00 100.00 Total (RAW) 99.07 99.64 99.03 98.05 98.36 98.37 98.00

LA-ICP-MS (ppm) Si29 14139638.35 13805940.83 12395628.55 11930137.10 Ca43 0.15 0.19 0.16 0.28 Sc45 8.25 6.83 11.12 3.87 Ti47 1826.69 1206.48 1781.37 607.82 Rb85 227.38 126.33 277.98 191.10 Sr88 14.14 10.17 11.42 8.68 Y89 30.59 30.74 53.17 28.69 Zr90 225.16 158.25 278.20 124.93 Nb93 38.09 51.45 79.35 34.35 Cs133 5.95 2.19 6.51 3.63 Ba138 490.53 393.33 417.91 409.41 La139 70.61 45.39 119.37 37.14 Ce140 125.98 95.70 226.29 89.30 Pr141 13.29 8.46 31.69 7.67 Nd146 57.10 31.26 124.11 27.82 Sm147 10.15 6.50 22.93 5.91 Eu151 0.75 0.43 0.93 0.67 Gd157 9.58 5.82 16.63 4.92 Tb159 1.98 1.19 2.35 0.85 Dy163 11.06 7.13 15.68 5.03 Ho165 1.82 1.52 2.35 1.06 Er166 4.53 3.96 5.62 2.92 Tm169 0.52 0.56 0.75 0.41 Yb172 3.21 3.35 5.15 2.51 Lu175 0.44 0.57 0.78 0.42 Hf178 7.01 5.35 7.49 3.95 Ta181 3.33 2.50 3.75 1.83 Pb208 47.58 46.64 58.13 35.16 Th232 23.46 22.07 51.69 12.94 U238 4.99 8.36 9.12 4.93

276 unit DRF DRF DRF DRF DRF DRF DRF DRF sample 08CP09 08CP09 08CP09 08CP09 08CP09 08CP09 08CP09 08CP09 description glass 3 glass 3 glass 3 glass 3 glass 3 glass 3 glass 3 glass 3 date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 352 353 354 355 356 357 358 359 TiO2 Oxide % 0.11 0.09 0.10 0.08 0.13 0.06 0.07 0.14 MgO Oxide % 0.08 0.05 0.06 0.08 0.06 0.05 0.07 0.07 MnO Oxide % 0.05 0.05 0.00 0.03 0.05 0.03 0.01 0.06 CaO Oxide % 0.40 0.42 0.46 0.44 0.47 0.41 0.38 0.34 K2O Oxide % 5.39 5.39 5.52 5.47 5.33 5.57 5.56 5.39 SiO2 Oxide % 76.59 76.67 77.20 77.21 77.06 77.21 76.27 76.82 Al2O3 Oxide % 12.17 11.84 12.09 12.04 12.25 12.10 11.97 12.10 FeO Oxide % 1.41 1.63 0.73 0.77 0.82 0.78 1.89 1.35 Na2O Oxide % 3.79 3.86 3.86 3.87 3.82 3.78 3.79 3.72 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 98.20 98.16 98.00 98.63 97.93 98.55 97.56 97.69

LA-ICP-MS (ppm) Si29 5979529.62 Ca43 0.39 Sc45 4.41 Ti47 677.95 Rb85 213.33 Sr88 9.42 Y89 36.19 Zr90 152.26 Nb93 39.10 Cs133 4.02 Ba138 433.09 La139 46.11 Ce140 103.55 Pr141 9.33 Nd146 34.10 Sm147 7.35 Eu151 0.41 Gd157 6.01 Tb159 1.03 Dy163 6.31 Ho165 1.32 Er166 3.57 Tm169 0.49 Yb172 3.09 Lu175 0.52 Hf178 5.09 Ta181 2.07 Pb208 35.21 Th232 14.92 U238 5.43

277 unit DRF DRF DRF DRF DRF sample 08CP09 08CP09 08CP09 08CP09 08CP09 description glass 3 glass z transect glass z transect glass z transect glass z transect date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 360 361 362 363 364 TiO2 Oxide % 0.11 0.07 0.10 0.09 0.10 MgO Oxide % 0.03 0.07 0.08 0.06 0.04 MnO Oxide % 0.01 0.03 0.03 0.00 0.08 CaO Oxide % 0.47 0.43 0.43 0.46 0.40 K2O Oxide % 5.54 5.51 5.57 5.51 5.55 SiO2 Oxide % 77.28 76.67 76.99 77.14 76.97 Al2O3 Oxide % 12.04 11.92 12.05 12.10 12.13 FeO Oxide % 0.74 1.35 0.81 0.79 0.88 Na2O Oxide % 3.78 3.94 3.93 3.85 3.85 P205 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 Total (RAW) 97.52 97.96 98.45 97.92 98.17

LA-ICP-MS (ppm) Si29 9583175.94 Ca43 0.27 Sc45 4.65 Ti47 587.42 Rb85 182.60 Sr88 8.63 Y89 32.73 Zr90 138.70 Nb93 33.51 Cs133 3.40 Ba138 392.16 La139 40.12 Ce140 86.84 Pr141 7.89 Nd146 30.42 Sm147 6.11 Eu151 0.30 Gd157 5.54 Tb159 0.96 Dy163 5.91 Ho165 1.16 Er166 3.21 Tm169 0.48 Yb172 2.77 Lu175 0.47 Hf178 4.67 Ta181 1.83 Pb208 29.73 Th232 13.91 U238 4.64

278 unit DRF DRF DRF DRF DRF sample 08CP09 08CP09 08CP09 08CP09 08CP09 description glass z transect glass z transect glass z transect glass z transect glass z transect date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 365 366 367 368 369 TiO2 Oxide % 0.06 0.08 0.09 0.12 0.10 MgO Oxide % 0.05 0.06 0.04 0.05 0.05 MnO Oxide % 0.04 0.03 0.00 0.03 0.01 CaO Oxide % 0.41 0.45 0.47 0.44 0.42 K2O Oxide % 5.47 5.61 5.60 5.47 5.29 SiO2 Oxide % 76.93 76.93 77.02 76.91 76.88 Al2O3 Oxide % 12.03 12.29 12.16 11.96 12.25 FeO Oxide % 1.27 0.78 0.82 1.26 1.24 Na2O Oxide % 3.75 3.76 3.81 3.77 3.75 P205 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.02 100.00 100.00 Total (RAW) 98.33 98.22 97.54 98.44 98.36

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

279 unit DRF DRF DRF DRF DRF sample 08CP09 08CP09 08CP09 08CP09 08CP09 description glass z transect glass z transect glass z transect glass z transect glass z transect date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 370 371 372 373 374 TiO2 Oxide % 0.09 0.11 0.06 0.08 0.08 MgO Oxide % 0.04 0.06 0.05 0.04 0.01 MnO Oxide % 0.08 0.04 0.07 0.07 0.05 CaO Oxide % 0.44 0.39 0.46 0.43 0.42 K2O Oxide % 5.61 5.48 5.58 5.31 5.52 SiO2 Oxide % 76.79 76.79 77.18 77.28 76.82 Al2O3 Oxide % 12.13 12.08 12.01 12.15 12.04 FeO Oxide % 0.95 1.26 0.76 0.86 1.15 Na2O Oxide % 3.86 3.78 3.82 3.78 3.91 P205 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 Total (RAW) 98.38 98.26 98.46 97.83 98.54

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

280

APPENDIX I

RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF GLASS FEATURES FROM THE EUBM

unit TUTT TUTT TUTT TUTT TUTT TUTT TUTT TUTT sample 0922 0922 0922 0922 0922 0922 0922 0922 description pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 197 198 199 200 201 202 203 204 TiO2 Oxide % 0.23 0.19 0.12 0.22 0.23 0.20 0.15 0.15 MgO Oxide % 0.01 0.00 0.01 0.04 0.00 0.00 0.01 0.00 MnO Oxide % 0.01 0.01 0.00 0.04 0.07 0.08 0.03 0.00 CaO Oxide % 0.24 0.21 0.23 0.30 0.27 0.25 0.30 0.23 K2O Oxide % 6.53 6.59 6.47 6.61 6.50 6.48 6.69 6.00 SiO2 Oxide % 77.79 78.14 78.15 77.77 78.02 77.59 77.96 78.30 Al2O3 Oxide % 12.16 11.89 12.02 11.98 12.14 12.23 11.93 12.11 FeO Oxide % 0.55 0.54 0.52 0.67 0.54 0.59 0.54 0.55 Na2O Oxide % 2.48 2.43 2.48 2.37 2.22 2.59 2.38 2.66 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 97.37 96.77 96.85 96.22 96.87 96.85 96.79 96.72

LA-ICP-MS (ppm) Si29 7478929.83 7894434.96 Ca43 0.32 0.24 Sc45 11.05 10.00 Ti47 1537.62 1457.80 Rb85 407.18 326.70 Sr88 14.15 13.81 Y89 44.85 41.80 Zr90 205.76 186.86 Nb93 62.66 57.92 Cs133 6.65 5.15 Ba138 497.76 463.97 La139 59.09 54.62 Ce140 134.96 124.67 Pr141 12.52 11.20 Nd146 46.77 42.61 Sm147 9.94 8.64 Eu151 0.89 0.71 Gd157 8.22 7.57 Tb159 1.33 1.13 Dy163 7.98 7.37 Ho165 1.68 1.54 Er166 4.72 4.25 Tm169 0.67 0.60 Yb172 4.79 3.68 Lu175 0.66 0.62 Hf178 6.34 5.42 Ta181 3.01 2.80 Pb208 44.79 39.03 Th232 18.48 16.92 U238 8.37 7.30

282 unit TUTT TUTT TUTT TUTT TUTT TUTT TUTT TUTT sample 0922 0922 0922 0922 0922 0922 0922 0922 description pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 252 253 254 255 256 257 258 259 TiO2 Oxide % 0.23 0.22 0.22 0.18 0.15 0.18 0.24 0.23 MgO Oxide % 0.01 0.00 0.00 0.00 0.00 0.02 0.00 0.01 MnO Oxide % 0.04 0.05 0.06 0.02 0.00 0.00 0.03 0.02 CaO Oxide % 0.28 0.30 0.23 0.23 0.29 0.25 0.30 0.27 K2O Oxide % 6.19 6.15 5.92 6.10 6.18 6.01 6.02 6.19 SiO2 Oxide % 77.13 77.94 78.27 77.89 78.02 78.01 77.58 77.18 Al2O3 Oxide % 11.91 12.02 11.90 12.08 12.00 12.05 11.89 12.25 FeO Oxide % 1.47 0.73 1.02 0.79 0.83 0.90 1.31 1.23 Na2O Oxide % 2.72 2.59 2.37 2.72 2.52 2.59 2.63 2.63 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 95.81 96.80 96.41 96.58 96.35 96.62 96.68 96.30

LA-ICP-MS (ppm) Si29 Ca43 Sc45 Ti47 Rb85 Sr88 Y89 Zr90 Nb93 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Dy163 Ho165 Er166 Tm169 Yb172 Lu175 Hf178 Ta181 Pb208 Th232 U238

283 unit TUTT TUTT TUTT TUTT TUTT TUTT TUTT sample 0922 0922 0922 0922 0922 0922 0922 description pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 pumice 2 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 260 261 262 263 264 265 266 TiO2 Oxide % 0.25 0.20 0.19 0.15 0.21 0.19 0.18 MgO Oxide % 0.15 0.01 0.03 0.04 0.00 0.03 0.03 MnO Oxide % 0.03 0.04 0.11 0.01 0.01 0.00 0.02 CaO Oxide % 0.79 0.27 0.32 0.30 0.30 0.28 0.30 K2O Oxide % 6.16 5.27 5.99 6.06 5.91 6.28 6.28 SiO2 Oxide % 77.09 80.45 77.91 78.26 78.42 77.93 77.84 Al2O3 Oxide % 12.01 11.09 12.31 12.04 12.13 12.05 11.97 FeO Oxide % 1.12 0.71 0.83 0.95 0.81 0.75 0.79 Na2O Oxide % 2.39 1.96 2.31 2.19 2.21 2.50 2.59 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 96.31 96.28 96.41 96.26 96.28 96.02 96.93

LA-ICP-MS (ppm) Si29 10759791.10 10812664.42 Ca43 0.19 0.28 Sc45 9.75 10.07 Ti47 1509.27 1517.18 Rb85 238.40 233.98 Sr88 15.53 15.82 Y89 39.63 39.88 Zr90 194.29 192.85 Nb93 59.16 58.45 Cs133 6.53 6.03 Ba138 493.80 481.41 La139 55.37 54.91 Ce140 127.89 126.89 Pr141 11.33 11.16 Nd146 42.01 41.67 Sm147 8.19 8.70 Eu151 0.68 0.69 Gd157 7.22 7.48 Tb159 1.29 1.22 Dy163 7.49 7.47 Ho165 1.60 1.56 Er166 4.33 4.38 Tm169 0.59 0.65 Yb172 4.01 3.86 Lu175 0.62 0.63 Hf178 5.70 5.69 Ta181 2.84 2.81 Pb208 39.35 39.21 Th232 18.16 18.00 U238 7.27 7.58

284 unit TUTT TUTT TUTT TUTT TUTT TUTT sample 0922 0922 0922 0922 0922 0922 description banded glass 1 banded glass 1 banded glass 1 banded glass 1 banded glass 1 banded glass 1 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 237 238 239 240 241 242 TiO2 Oxide % 0.13 0.14 0.13 0.13 0.12 0.12 MgO Oxide % 0.05 0.02 0.04 0.03 0.03 0.09 MnO Oxide % 0.07 0.05 0.02 0.02 0.04 0.01 CaO Oxide % 0.50 0.48 0.46 0.46 0.53 0.55 K2O Oxide % 5.26 5.76 5.69 5.48 5.12 5.52 SiO2 Oxide % 78.47 78.39 78.53 78.80 79.01 78.09 Al2O3 Oxide % 12.18 12.15 12.18 12.18 12.22 12.06 FeO Oxide % 1.58 1.22 1.21 1.14 1.30 1.62 Na2O Oxide % 1.76 1.80 1.75 1.76 1.62 1.95 P205 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 93.15 93.96 93.49 93.29 93.24 93.84

LA-ICP-MS (ppm) Si29 10066044.56 Ca43 0.26 Sc45 8.79 Ti47 952.59 Rb85 257.64 Sr88 4.57 Y89 46.92 Zr90 174.31 Nb93 58.11 Cs133 7.03 Ba138 107.10 La139 65.42 Ce140 133.04 Pr141 12.58 Nd146 47.36 Sm147 9.51 Eu151 0.41 Gd157 8.01 Tb159 1.46 Dy163 8.53 Ho165 1.77 Er166 4.91 Tm169 0.75 Yb172 4.44 Lu175 0.67 Hf178 6.07 Ta181 3.01 Pb208 30.11 Th232 20.94 U238 6.86

285 unit TUTT TUTT TUTT TUTT TUTT TUTT TUTT sample 0922 0922 0922 0922 0922 0922 0922 description banded glass 1 banded glass 2 banded glass 2 banded glass 2 banded glass 2 banded glass 2 banded glass 2 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 243 244 245 246 247 248 249 TiO2 Oxide % 0.10 0.13 0.11 0.16 0.08 0.14 0.13 MgO Oxide % 0.05 0.03 0.04 0.03 0.07 0.05 0.04 MnO Oxide % 0.04 0.03 0.05 0.06 0.03 0.04 0.02 CaO Oxide % 0.43 0.46 0.52 0.51 0.59 0.44 0.48 K2O Oxide % 5.39 5.54 5.67 5.80 5.47 5.97 5.48 SiO2 Oxide % 78.66 78.38 78.03 78.19 78.46 77.33 78.33 Al2O3 Oxide % 12.17 12.05 12.26 11.99 12.09 11.97 12.27 FeO Oxide % 1.35 1.46 1.28 1.12 1.32 1.74 1.33 Na2O Oxide % 1.80 1.93 2.05 2.15 1.89 2.31 1.92 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 94.00 94.62 93.99 94.42 94.06 94.40 94.32

LA-ICP-MS (ppm) Si29 10038026.28 8647550.81 Ca43 0.29 0.25 Sc45 8.46 8.57 Ti47 981.36 972.11 Rb85 282.37 244.43 Sr88 4.63 4.58 Y89 47.56 42.54 Zr90 176.66 165.53 Nb93 55.43 58.30 Cs133 7.89 7.00 Ba138 107.83 109.44 La139 64.48 61.40 Ce140 134.73 133.83 Pr141 12.94 12.16 Nd146 47.84 45.33 Sm147 9.34 8.55 Eu151 0.40 0.40 Gd157 7.76 7.84 Tb159 1.42 1.29 Dy163 8.93 8.18 Ho165 1.83 1.61 Er166 5.24 4.66 Tm169 0.72 0.64 Yb172 4.50 4.47 Lu175 0.72 0.63 Hf178 6.17 5.53 Ta181 3.13 3.02 Pb208 32.92 33.77 Th232 21.90 20.07 U238 7.16 7.19

286 unit TUTT TUTT CAN CAN CAN CAN CAN CAN CAN sample 0922 0922 0934 0934 0934 0934 0934 0934 0934 description banded glass 2 banded glass 2 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 250 251 113 114 115 116 117 118 119 TiO2 Oxide % 0.12 0.13 0.24 0.17 0.22 0.20 0.17 0.20 0.22 MgO Oxide % 0.05 0.04 0.09 0.09 0.08 0.08 0.08 0.04 0.08 MnO Oxide % 0.01 0.07 0.03 0.01 0.09 0.07 0.06 0.08 0.05 CaO Oxide % 0.50 0.43 0.44 0.53 0.54 0.52 0.53 0.32 0.52 K2O Oxide % 5.69 5.89 5.35 5.32 5.40 5.47 5.33 5.46 5.40 SiO2 Oxide % 78.22 77.76 77.02 77.16 77.49 77.38 77.75 78.24 77.72 Al2O3 Oxide % 12.08 12.03 11.95 11.99 11.95 11.89 11.86 11.95 11.85 FeO Oxide % 1.26 1.49 1.88 1.64 1.27 1.24 1.19 0.63 1.15 Na2O Oxide % 2.08 2.17 2.99 3.08 2.95 3.14 3.02 3.08 3.01 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 94.08 94.54 97.71 96.93 97.36 97.39 98.17 97.42 97.43

LA-ICP-MS (ppm) Si29 8530683.38 Ca43 0.25 Sc45 8.14 Ti47 932.26 Rb85 245.73 Sr88 4.85 Y89 40.93 Zr90 156.97 Nb93 54.68 Cs133 8.09 Ba138 110.51 La139 58.40 Ce140 126.63 Pr141 11.54 Nd146 42.49 Sm147 8.53 Eu151 0.40 Gd157 7.53 Tb159 1.26 Dy163 7.71 Ho165 1.54 Er166 4.48 Tm169 0.63 Yb172 4.05 Lu175 0.62 Hf178 5.69 Ta181 2.84 Pb208 33.40 Th232 19.16 U238 7.04

287 unit CAN CAN CAN CAN CAN CAN CAN CAN CAN CAN sample 0934 0934 0934 0934 0934 0934 0934 0934 0934 0934 description pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 pumice 1 date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 Line Numbers 120 121 122 123 124 125 126 127 128 129 TiO2 Oxide % 0.19 0.15 0.21 0.20 0.16 0.23 0.20 0.24 0.24 0.22 MgO Oxide % 0.07 0.10 0.08 0.06 0.09 0.07 0.07 0.09 0.07 0.09 MnO Oxide % 0.08 0.04 0.03 0.04 0.04 0.00 0.02 0.00 0.03 0.02 CaO Oxide % 0.48 0.44 0.41 0.54 0.46 0.49 0.54 0.48 0.44 0.46 K2O Oxide % 5.33 5.61 5.40 5.60 5.50 5.47 5.43 5.32 5.44 5.47 SiO2 Oxide % 77.59 77.63 77.46 77.26 77.51 77.36 77.46 77.62 77.53 77.61 Al2O3 Oxide % 11.94 11.90 11.98 12.02 11.81 12.06 11.94 12.12 11.95 11.88 FeO Oxide % 1.30 1.13 1.30 1.31 1.33 1.30 1.31 1.09 1.27 1.08 Na2O Oxide % 3.01 2.99 3.12 2.97 3.08 3.02 3.01 3.03 3.04 3.16 P205 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Total (RAW) 97.52 97.66 97.32 97.83 97.52 97.40 97.34 97.19 97.36 97.30

LA-ICP-MS (ppm) 0934 pumice1 0934 pumice 1b Si29 16912740.84 16521806.60 Ca43 0.31 0.30 Sc45 10.47 10.01 Ti47 1470.80 1441.24 Rb85 208.97 218.03 Sr88 17.30 16.37 Y89 44.95 43.78 Zr90 197.41 194.90 Nb93 60.22 58.91 Cs133 5.33 4.81 Ba138 535.19 493.89 La139 60.76 57.07 Ce140 126.36 121.40 Pr141 12.33 11.71 Nd146 47.33 44.19 Sm147 9.27 8.50 Eu151 0.89 0.86 Gd157 8.47 7.86 Tb159 1.42 1.22 Dy163 8.35 7.72 Ho165 1.70 1.56 Er166 4.81 4.40 Tm169 0.71 0.62 Yb172 4.41 4.02 Lu175 0.75 0.62 Hf178 6.07 5.83 Ta181 2.99 2.91 Pb208 33.70 36.24 Th232 18.61 18.06 U238 6.92 6.74

288 unit CAN CAN DRF DRF sample 0934 0934 08CP01B 08CP01B description pumice 1 pumice 1 ribbon inbetween ribbons date 11/9/2009 11/9/2009 7/13/2009 7/13/2009 Line Numbers 130 131 426 427 TiO2 Oxide % 0.19 0.17 0.11 0.10 MgO Oxide % 0.06 0.08 0.06 0.06 MnO Oxide % 0.04 0.06 0.06 0.00 CaO Oxide % 0.53 0.50 0.37 0.38 K2O Oxide % 5.39 5.67 5.27 5.36 SiO2 Oxide % 77.50 77.75 76.51 77.94 Al2O3 Oxide % 12.07 11.97 12.14 12.15 FeO Oxide % 1.14 1.04 1.81 0.48 Na2O Oxide % 3.09 2.77 3.66 3.52 P205 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 Total (RAW) 97.54 97.66 98.31 98.07

LA-ICP-MS (ppm) Si29 9337707.39 11099763.11 10038424.42 9528444.17 Ca43 0.25 0.28 0.29 0.25 Sc45 2.68 4.11 3.76 4.06 Ti47 619.59 638.44 653.78 634.22 Rb85 197.20 193.95 197.99 200.80 Sr88 7.66 8.45 8.57 7.77 Y89 28.52 28.43 30.91 29.03 Zr90 124.28 124.55 132.73 126.60 Nb93 35.07 34.42 36.22 35.59 Cs133 3.57 3.52 3.69 3.84 Ba138 380.48 392.35 405.58 377.52 La139 36.29 36.57 39.41 37.20 Ce140 89.51 89.97 93.89 90.41 Pr141 7.52 7.61 8.05 7.74 Nd146 28.00 28.02 29.56 27.86 Sm147 5.49 5.77 6.27 5.77 Eu151 0.37 0.38 0.40 0.33 Gd157 4.98 4.87 4.99 5.02 Tb159 0.82 0.82 0.85 0.87 Dy163 5.03 5.05 5.31 5.13 Ho165 1.04 1.00 1.12 1.00 Er166 2.76 2.85 3.05 2.74 Tm169 0.42 0.43 0.43 0.43 Yb172 2.63 2.50 2.76 2.66 Lu175 0.41 0.40 0.45 0.42 Hf178 4.12 4.14 4.47 4.28 Ta181 1.80 1.85 1.95 1.85 Pb208 33.10 34.17 35.69 33.35 Th232 12.53 12.65 13.45 12.67 U238 4.97 4.84 5.06 5.11

289 unit DRF DRF DRF DRF sample 08CP09 08CP09 08CP09 08CP09 description dust 1 dust 1 dust 1 dust date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 Line Numbers 338 339 340 381 TiO2 Oxide % 0.11 0.10 0.09 0.07 MgO Oxide % 0.06 0.05 0.04 0.04 MnO Oxide % 0.01 0.01 0.06 0.01 CaO Oxide % 0.51 0.47 0.42 0.46 K2O Oxide % 5.52 5.58 5.49 5.65 SiO2 Oxide % 76.91 77.00 77.06 76.90 Al2O3 Oxide % 11.97 11.96 11.84 11.85 FeO Oxide % 1.06 1.11 1.05 1.10 Na2O Oxide % 3.83 3.70 3.94 3.91 P205 0.00 0.00 0.00 0.00 CI 0.00 0.00 0.00 0.00 Totals 100.00 100.00 100.00 100.00 Total (RAW) 97.74 97.27 97.48 97.76

LA-ICP-MS (ppm) Si29 9547753.17 8701677.75 8009940.17 6328368.16 9422479.98 Ca43 0.25 0.31 0.34 0.31 0.32 Sc45 3.66 4.67 5.92 2.73 4.61 Ti47 616.21 566.25 639.50 661.49 632.42 Rb85 193.41 193.44 212.57 222.92 224.53 Sr88 7.84 7.13 8.08 8.35 7.37 Y89 31.10 28.51 32.20 31.80 32.51 Zr90 130.70 114.97 128.41 137.76 123.62 Nb93 34.52 32.10 36.24 38.72 36.32 Cs133 3.69 3.90 4.58 4.28 4.34 Ba138 373.76 342.27 382.35 408.42 368.10 La139 37.93 35.72 40.42 41.18 40.10 Ce140 88.63 87.61 96.58 98.50 96.63 Pr141 7.64 7.44 8.41 8.45 8.21 Nd146 28.77 27.82 31.36 31.07 30.70 Sm147 5.98 5.96 6.27 6.16 6.39 Eu151 0.36 0.43 0.50 0.48 0.44 Gd157 5.01 4.78 5.54 5.36 5.58 Tb159 0.93 0.83 0.92 0.95 0.94 Dy163 5.26 4.93 5.64 5.41 5.73 Ho165 1.06 1.00 1.14 1.11 1.19 Er166 3.01 2.90 3.10 3.17 3.29 Tm169 0.47 0.39 0.43 0.42 0.47 Yb172 2.72 2.59 2.78 3.01 2.78 Lu175 0.42 0.40 0.44 0.43 0.46 Hf178 4.46 3.95 4.45 4.36 4.13 Ta181 1.80 1.63 1.78 1.94 1.73 Pb208 33.75 36.29 42.65 41.10 42.94 Th232 13.22 11.86 12.95 14.19 12.65 U238 4.93 5.30 6.07 6.09 5.95

290

APPENDIX J

RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF PLAGIOCLASE FROM THE EUBM

Unit TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral p ppppp p p c/i/r r r c r c c r r Line Numbers 25 26 27 28 29 30 31 32 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 7.55 7.48 7.43 8.30 7.17 7.69 7.52 7.64 Al2O3 Oxide Percents 22.60 23.41 22.76 22.85 24.11 23.01 23.76 23.40 SiO2 Oxide Percents 62.43 61.29 62.65 62.01 60.60 62.77 62.53 63.23 K2O Oxide Percents 2.37 1.51 1.96 1.49 1.18 1.64 1.64 2.04 FeO Oxide Percents 0.29 0.29 0.30 0.31 0.29 0.29 0.34 0.32 BaO Oxide Percents 0.34 0.24 0.22 0.15 0.19 0.30 0.14 0.28 CaO Oxide Percents 3.94 5.06 4.17 4.41 6.04 4.40 4.88 4.39 Oxide Totals 99.51 99.30 99.49 99.52 99.60 100.11 100.81 101.31

Na Formula Atoms 0.66 0.65 0.64 0.72 0.62 0.66 0.64 0.65 Al Formula Atoms 1.20 1.24 1.20 1.21 1.27 1.21 1.24 1.21 Si Formula Atoms 2.80 2.76 2.80 2.78 2.72 2.79 2.76 2.79 K Formula Atoms 0.14 0.09 0.11 0.09 0.07 0.09 0.09 0.11 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.01 0.00 0.00 0.00 0.00 0.01 0.00 0.00 Ca Formula Atoms 0.19 0.24 0.20 0.21 0.29 0.21 0.23 0.21 Formula Totals 13.00 12.99 12.97 13.02 12.99 12.98 12.99 12.99 100*Ca/(Ca+Na) 22.36 27.22 23.65 22.68 31.77 24.02 26.42 24.11

An 19.27 24.82 20.88 20.79 29.58 21.70 23.89 21.27 Ab 66.91 66.35 67.43 70.85 63.53 68.64 66.55 66.96 Or 13.81 8.83 11.68 8.36 6.89 9.66 9.56 11.76

Grain Average An 21.66 25.18 22.80 21.27 Ab 66.90 67.19 67.60 66.96 Or 11.44 7.63 9.61 11.76

LA-ICP-MS (ppm) c Si29 38483926.00 Mg25 89.25 Ca43 3.88 Ti47 170.41 Rb85 5.85 Sr88 435.63 Y89 0.60 Cs133 0.01 Ba138 1825 La139 26.41 Ce140 33.21 Pr141 2.33 Nd146 6.63 Sm147 0.66 Eu151 6.76 Gd157 0.55 Tb159 0.03 Pb208 22.21

292 Unit TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral p p pppp p p c/i/r crriic i r Line Numbers 35 36 95 96 97 98 99 100 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 7.63 7.63 7.79 7.41 6.79 7.08 7.36 7.39 Al2O3 Oxide Percents 22.80 23.04 22.51 24.07 25.01 24.31 23.90 23.70 SiO2 Oxide Percents 62.25 62.78 63.09 60.71 59.56 60.85 61.96 61.43 K2O Oxide Percents 2.09 1.81 1.77 1.36 1.02 1.16 1.33 1.25 FeO Oxide Percents 0.33 0.31 0.33 0.33 0.31 0.40 0.37 0.40 BaO Oxide Percents 0.39 0.29 0.22 0.13 0.12 0.14 0.19 0.11 CaO Oxide Percents 4.29 4.43 4.11 5.78 6.67 5.90 5.36 5.54 Oxide Totals 99.80 100.27 99.80 99.79 99.47 99.84 100.47 99.82

Na Formula Atoms 0.66 0.66 0.67 0.64 0.59 0.61 0.63 0.64 Al Formula Atoms 1.20 1.21 1.18 1.27 1.32 1.28 1.25 1.25 Si Formula Atoms 2.79 2.79 2.81 2.72 2.68 2.72 2.75 2.75 K Formula Atoms 0.12 0.10 0.10 0.08 0.06 0.07 0.08 0.07 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.02 0.01 0.01 Ba Formula Atoms 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.21 0.21 0.20 0.28 0.32 0.28 0.26 0.27 Formula Totals 13.00 12.99 12.98 13.00 12.99 12.98 12.98 12.99 100*Ca/(Ca+Na) 23.71 24.28 22.59 30.11 35.17 31.54 28.70 29.29

An 20.84 21.71 20.25 27.77 33.06 29.37 26.46 27.15 Ab 67.06 67.74 69.38 64.46 60.94 63.74 65.73 65.53 Or 12.10 10.55 10.38 7.77 6.00 6.89 7.80 7.32

Grain Average 21.28 27.34 67.40 64.96 11.32 7.69

LA-ICP-MS (ppm) rc Si29 38180914.85 39076300.20 Mg25 98.17 105.98 Ca43 4.21 4.88 Ti47 192.96 204.06 Rb85 4.56 2.53 Sr88 374.22 480.78 Y89 0.39 0.47 Cs133 0.00 0.01 Ba138 1019 904 La139 14.34 14.86 Ce140 23.64 25.01 Pr141 1.60 1.75 Nd146 4.65 4.90 Sm147 0.54 0.53 Eu151 5.64 6.50 Gd157 0.32 0.42 Tb159 0.03 0.03 Pb208 18.92 16.26

293 Unit TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral pp p p ppp c/i/r ic i r icr Line Numbers 129 130 131 132 133 134 135 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 7.51 7.32 6.95 7.86 7.58 7.60 7.62 Al2O3 Oxide Percents 23.55 24.11 24.47 22.49 22.82 23.38 23.66 SiO2 Oxide Percents 62.00 61.47 60.96 63.70 62.71 62.25 61.82 K2O Oxide Percents 1.38 1.26 1.06 1.85 1.93 1.56 1.47 FeO Oxide Percents 0.35 0.35 0.32 0.32 0.31 0.33 0.33 BaO Oxide Percents 0.17 0.22 0.13 0.22 0.34 0.23 0.28 CaO Oxide Percents 5.10 5.80 5.79 3.88 4.31 4.98 5.00 Oxide Totals 100.06 100.53 99.67 100.32 100.01 100.32 100.19

Na Formula Atoms 0.65 0.63 0.60 0.68 0.66 0.65 0.66 Al Formula Atoms 1.24 1.26 1.29 1.17 1.20 1.23 1.24 Si Formula Atoms 2.76 2.73 2.72 2.82 2.80 2.77 2.75 K Formula Atoms 0.08 0.07 0.06 0.10 0.11 0.09 0.08 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.00 0.01 0.00 0.00 Ca Formula Atoms 0.24 0.28 0.28 0.18 0.21 0.24 0.24 Formula Totals 12.98 12.99 12.96 12.98 12.99 12.99 12.99 100*Ca/(Ca+Na) 27.30 30.45 31.54 21.42 23.89 26.60 26.62

An 25.10 28.22 29.51 19.10 21.19 24.20 24.35 Ab 66.84 64.46 64.05 70.06 67.50 66.79 67.13 Or 8.06 7.32 6.44 10.83 11.31 9.01 8.52

Grain Average 25.48 23.25 66.35 67.14 8.16 9.61

LA-ICP-MS (ppm) rc Si29 43303619.43 40987791.98 Mg25 325.49 114.46 Ca43 4.06 3.98 Ti47 203.00 184.87 Rb85 9.71 4.15 Sr88 451.13 427.16 Y89 2.95 0.47 Cs133 0.09 0.01 Ba138 1681 1439 La139 27.08 19.54 Ce140 41.92 28.25 Pr141 2.83 1.90 Nd146 10.43 5.25 Sm147 1.26 0.50 Eu151 7.36 5.76 Gd157 0.96 0.35 Tb159 0.11 0.03 Pb208 22.93 19.90

294 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 mineral pppppppppp c/i/r rcrrircrrc Line Numbers 136 137 143 147 151 152 153 154 155 156 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 7.51 7.51 7.53 7.17 6.63 7.84 7.51 7.69 7.67 6.83 Al2O3 Oxide Percents 23.28 23.52 22.97 22.78 26.22 22.63 23.88 22.96 24.05 25.53 SiO2 Oxide Percents 63.00 62.12 62.72 62.17 58.92 63.45 61.38 62.94 61.68 58.79 K2O Oxide Percents 1.72 1.69 1.75 2.16 0.77 1.90 1.33 1.92 1.40 0.82 FeO Oxide Percents 0.32 0.27 0.33 0.34 0.32 0.31 0.32 0.33 0.33 0.32 BaO Oxide Percents 0.22 0.27 0.24 0.30 0.06 0.27 0.26 0.30 0.23 0.13 CaO Oxide Percents 4.68 5.09 4.45 4.54 7.85 4.02 5.29 4.41 5.44 7.15 Oxide Totals 100.74 100.47 100.01 99.45 100.76 100.43 99.97 100.54 100.80 99.57

Na Formula Atoms 0.64 0.65 0.65 0.62 0.57 0.67 0.65 0.66 0.66 0.60 Al Formula Atoms 1.21 1.23 1.21 1.21 1.38 1.18 1.26 1.20 1.26 1.35 Si Formula Atoms 2.79 2.76 2.79 2.79 2.62 2.81 2.74 2.79 2.74 2.64 K Formula Atoms 0.10 0.10 0.10 0.12 0.04 0.11 0.08 0.11 0.08 0.05 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.01 0.00 0.00 0.00 0.01 0.00 0.00 Ca Formula Atoms 0.22 0.24 0.21 0.22 0.37 0.19 0.25 0.21 0.26 0.34 Formula Totals 12.98 12.99 12.98 12.98 13.00 12.99 12.99 12.99 13.01 13.00 100*Ca/(Ca+Na) 25.62 27.27 24.63 25.90 39.55 22.07 28.00 24.05 28.16 36.64

An 23.04 24.62 22.08 22.59 37.81 19.63 25.82 21.37 25.92 34.89 Ab 66.88 65.67 67.57 64.63 57.78 69.32 66.42 67.51 66.13 60.34 Or 10.08 9.72 10.36 12.78 4.40 11.05 7.76 11.12 7.95 4.77

Grain Average 23.83 22.08 22.59 37.81 22.28 30.40 66.27 67.57 64.63 57.78 67.75 63.24 9.90 10.36 12.78 4.40 9.98 6.36

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

295 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 mineral pppppppppp c/i/r rcrcrcrcrc Line Numbers 160 161 162 174 175 176 177 178 180 181 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 7.73 7.27 7.95 7.51 7.65 7.56 8.11 7.27 7.45 7.32 Al2O3 Oxide Percents 22.71 24.53 23.39 23.71 22.41 23.63 22.90 24.22 22.83 24.96 SiO2 Oxide Percents 62.99 60.71 62.72 61.74 63.24 62.47 63.34 61.46 62.85 60.75 K2O Oxide Percents 2.04 1.11 1.21 1.38 1.90 1.52 1.49 1.26 1.85 0.96 FeO Oxide Percents 0.35 0.34 0.36 0.36 0.32 0.31 0.33 0.34 0.31 0.40 BaO Oxide Percents 0.25 0.22 0.22 0.21 0.32 0.22 0.18 0.23 0.28 0.14 CaO Oxide Percents 4.32 6.02 4.69 4.88 3.81 5.17 4.16 5.39 4.30 6.49 Oxide Totals 100.38 100.21 100.54 99.79 99.64 100.89 100.50 100.17 99.87 101.03

Na Formula Atoms 0.67 0.63 0.68 0.65 0.66 0.65 0.70 0.63 0.64 0.63 Al Formula Atoms 1.19 1.29 1.22 1.25 1.18 1.23 1.19 1.27 1.20 1.30 Si Formula Atoms 2.80 2.71 2.78 2.76 2.82 2.76 2.80 2.74 2.80 2.69 K Formula Atoms 0.12 0.06 0.07 0.08 0.11 0.09 0.08 0.07 0.11 0.05 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.00 0.01 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.21 0.29 0.22 0.23 0.18 0.25 0.20 0.26 0.21 0.31 Formula Totals 13.00 12.99 12.99 12.98 12.97 12.99 12.99 12.98 12.97 13.00 100*Ca/(Ca+Na) 23.62 31.40 24.60 26.43 21.61 27.44 22.08 29.08 24.20 32.89

An 20.86 29.38 22.88 24.27 19.15 25.03 20.17 26.90 21.52 31.08 Ab 67.45 64.18 70.11 67.55 69.48 66.19 71.21 65.61 67.43 63.43 Or 11.69 6.44 7.02 8.18 11.37 8.78 8.62 7.49 11.04 5.49

Grain Average 25.12 22.88 24.27 22.09 23.54 26.30 65.82 70.11 67.55 67.83 68.41 65.43 9.07 7.02 8.18 10.08 8.05 8.26

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

296 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP03 07CP03 07CP03 07CP03 07CP03 07CP06 07CP06 07CP06 07CP06 07CP06 mineral ppppp ppppp c/i/r ricir rcrcr Line Numbers 196 197 198 199 200 254 255 256 257 258 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 7.67 7.51 7.59 7.96 7.11 7.82 6.99 7.77 7.80 7.60 Al2O3 Oxide Percents 22.67 23.38 22.57 23.24 24.62 22.50 24.66 23.24 22.79 22.72 SiO2 Oxide Percents 63.06 62.90 63.06 62.23 60.91 62.71 60.62 62.57 63.00 62.57 K2O Oxide Percents 2.24 2.02 2.04 1.27 1.17 2.09 0.95 1.44 1.78 2.11 FeO Oxide Percents 0.32 0.29 0.32 0.35 0.31 0.28 0.42 0.29 0.32 0.29 BaO Oxide Percents 0.20 0.30 0.27 0.14 0.18 0.33 0.12 0.20 0.24 0.28 CaO Oxide Percents 3.94 4.69 4.09 4.97 6.07 3.77 6.31 4.74 4.31 4.02 Oxide Totals 100.11 101.10 99.95 100.17 100.38 99.51 100.05 100.26 100.26 99.59

Na Formula Atoms 0.66 0.64 0.66 0.69 0.61 0.68 0.60 0.67 0.67 0.66 Al Formula Atoms 1.19 1.22 1.19 1.22 1.29 1.19 1.30 1.22 1.19 1.20 Si Formula Atoms 2.81 2.78 2.81 2.77 2.71 2.81 2.70 2.78 2.80 2.80 K Formula Atoms 0.13 0.11 0.12 0.07 0.07 0.12 0.05 0.08 0.10 0.12 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.02 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.01 0.00 0.00 0.00 0.01 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.19 0.22 0.20 0.24 0.29 0.18 0.30 0.23 0.21 0.19 Formula Totals 12.99 12.99 12.98 13.00 12.98 12.99 12.98 12.99 12.99 12.99 100*Ca/(Ca+Na) 22.12 25.64 22.95 25.65 32.03 21.06 33.30 25.23 23.41 22.63

An 19.24 22.65 20.20 23.80 29.82 18.49 31.43 23.12 20.99 19.84 Ab 67.75 65.70 67.83 68.98 63.30 69.30 62.96 68.53 68.67 67.80 Or 13.01 11.65 11.97 7.23 6.88 12.22 5.61 8.35 10.33 12.36

Grain Average 23.14 24.96 66.71 66.13 10.15 8.91

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

297 Unit TSC TSC TSC TSC CAN CAN CAN CAN CAN CAN Sample 07CP06 07CP06 07CP06 07CP06 0934 0934 0934 0934 0934 0934 mineral pppp pppppp c/i/r ccrc rriiii Line Numbers 259 260 261 262 56 57 58 59 60 61 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 6.88 7.13 7.71 7.51 7.82 7.71 7.44 7.58 7.75 7.58 Al2O3 Oxide Percents 25.22 24.80 22.78 23.40 23.32 23.85 24.55 24.29 23.65 23.87 SiO2 Oxide Percents 59.17 58.87 62.85 61.76 62.60 62.38 61.52 61.56 62.70 62.46 K2O Oxide Percents 1.01 1.05 2.15 1.56 1.49 1.48 1.15 1.16 1.71 1.40 FeO Oxide Percents 0.30 0.30 0.28 0.33 0.31 0.35 0.29 0.31 0.31 0.31 BaO Oxide Percents 0.14 0.15 0.31 0.19 0.18 0.21 0.18 0.16 0.25 0.17 CaO Oxide Percents 6.81 6.64 4.18 5.06 4.73 5.11 5.64 5.71 4.70 5.10 Oxide Totals 99.52 98.93 100.26 99.82 100.45 101.07 100.75 100.76 101.08 100.89

Na Formula Atoms 0.60 0.63 0.67 0.65 0.67 0.66 0.64 0.65 0.66 0.65 Al Formula Atoms 1.34 1.32 1.20 1.23 1.22 1.24 1.28 1.26 1.23 1.24 Si Formula Atoms 2.66 2.67 2.80 2.76 2.77 2.75 2.72 2.72 2.76 2.75 K Formula Atoms 0.06 0.06 0.12 0.09 0.08 0.08 0.06 0.07 0.10 0.08 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.03 0.04 0.03 0.03 0.03 0.03 Ba Formula Atoms 0.00 0.00 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.33 0.32 0.20 0.24 0.22 0.24 0.27 0.27 0.22 0.24 Formula Totals 13.00 13.01 13.00 12.99 13.00 13.01 13.00 13.01 13.01 12.99 100*Ca/(Ca+Na) 35.36 33.99 23.07 27.13 25.06 26.82 29.51 29.39 25.10 27.09

An 33.29 31.94 20.21 24.68 22.91 24.54 27.54 27.44 22.64 24.88 Ab 60.85 62.03 67.41 66.27 68.51 66.98 65.78 65.92 67.54 66.99 Or 5.87 6.02 12.38 9.06 8.58 8.48 6.68 6.64 9.82 8.13

Grain Average 25.84 22.44 65.58 66.84 8.59 10.72

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

298 Unit CAN CAN CAN CAN CAN CAN CAN CAN CAN CAN Sample 0934 0934 0934 0934 0934 0934 0934 0934 0934 0934 mineral pppppppppp c/i/r iiiiiicccc Line Numbers 62 63 64 65 66 67 68 69 70 71 Date

Na2O Oxide Percents 7.74 7.75 7.84 7.83 7.52 6.55 7.09 6.39 7.50 7.81 Al2O3 Oxide Percents 23.35 23.05 23.04 23.17 24.43 27.11 25.32 27.09 23.73 23.08 SiO2 Oxide Percents 62.61 62.75 63.35 62.86 61.91 57.90 60.01 57.65 62.16 63.10 K2O Oxide Percents 1.65 1.79 1.76 1.80 1.22 0.62 0.86 0.65 1.38 1.67 FeO Oxide Percents 0.30 0.31 0.32 0.27 0.28 0.31 0.31 0.29 0.27 0.31 BaO Oxide Percents 0.32 0.29 0.36 0.24 0.16 0.12 0.18 0.12 0.19 0.27 CaO Oxide Percents 4.65 4.39 4.47 4.34 5.49 8.43 6.94 8.24 5.02 4.32 Oxide Totals 100.62 100.33 101.14 100.51 101.01 101.05 100.70 100.44 100.25 100.56

Na Formula Atoms 0.66 0.67 0.67 0.67 0.64 0.56 0.61 0.55 0.64 0.67 Al Formula Atoms 1.22 1.20 1.19 1.21 1.27 1.42 1.32 1.42 1.24 1.20 Si Formula Atoms 2.77 2.78 2.79 2.78 2.73 2.57 2.66 2.57 2.75 2.79 K Formula Atoms 0.09 0.10 0.10 0.10 0.07 0.04 0.05 0.04 0.08 0.09 Fe Formula Atoms 0.03 0.03 0.04 0.03 0.03 0.03 0.03 0.03 0.03 0.03 Ba Formula Atoms 0.01 0.01 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.22 0.21 0.21 0.21 0.26 0.40 0.33 0.39 0.24 0.20 Formula Totals 13.00 13.00 13.00 13.00 13.00 13.02 13.01 13.01 12.99 12.99 100*Ca/(Ca+Na) 24.94 23.86 23.95 23.44 28.74 41.55 35.09 41.62 27.01 23.42

An 22.56 21.38 21.53 21.01 26.71 40.08 33.37 40.05 24.82 21.14 Ab 67.89 68.26 68.37 68.62 66.24 56.38 61.73 56.17 67.07 69.15 Or 9.55 10.36 10.11 10.37 7.05 3.54 4.91 3.79 8.11 9.71

Grain Average

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

299 Unit CAN CAN CAN CAN CAN CAN CAN CAN Sample 0934 0934 0934 0934 0934 0934 0934 0934 mineral pppppppp c/i/r ccciiirr Line Numbers 72 74 75 76 77 78 79 80 Date

Na2O Oxide Percents 7.77 8.18 7.99 7.73 7.88 7.84 7.72 7.77 Al2O3 Oxide Percents 22.96 22.95 22.93 23.44 23.45 23.24 23.43 23.59 SiO2 Oxide Percents 63.43 63.59 63.35 63.10 62.55 62.73 62.83 62.78 K2O Oxide Percents 1.66 1.55 1.77 1.56 1.54 1.60 1.58 1.60 FeO Oxide Percents 0.30 0.28 0.29 0.32 0.33 0.27 0.31 0.33 BaO Oxide Percents 0.24 0.39 0.27 0.24 0.24 0.25 0.24 0.19 CaO Oxide Percents 4.31 4.12 4.12 4.50 4.66 4.50 4.66 4.79 Oxide Totals 100.68 101.06 100.72 100.90 100.66 100.44 100.77 101.05

Na Formula Atoms 0.66 0.70 0.68 0.66 0.67 0.67 0.66 0.66 Al Formula Atoms 1.19 1.19 1.19 1.22 1.22 1.21 1.22 1.22 Si Formula Atoms 2.80 2.80 2.79 2.78 2.76 2.78 2.77 2.76 K Formula Atoms 0.09 0.09 0.10 0.09 0.09 0.09 0.09 0.09 Fe Formula Atoms 0.03 0.03 0.03 0.04 0.04 0.03 0.03 0.04 Ba Formula Atoms 0.00 0.01 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.20 0.19 0.19 0.21 0.22 0.21 0.22 0.23 Formula Totals 12.99 13.00 13.00 12.99 13.01 13.00 13.00 13.00 100*Ca/(Ca+Na) 23.47 21.76 22.18 24.35 24.63 24.10 25.04 25.43

An 21.19 19.82 19.93 22.13 22.46 21.87 22.74 23.10 Ab 69.10 71.28 69.91 68.75 68.71 68.86 68.07 67.74 Or 9.71 8.90 10.16 9.12 8.84 9.28 9.19 9.16

Grain Average 24.83 66.83 8.34

LA-ICP-MS (ppm) rrcc Si29 43275486.70 47540309.53 39100854.25 43825667.67 Mg25 83.41 79.33 10.21 75.05 Ca43 3.84 3.49 0.57 3.57 Ti47 165.17 182.32 23.69 169.63 Rb85 4.44 4.78 0.29 5.44 Sr88 408.21 413.70 44.41 423.05 Y89 0.88 0.87 0.11 0.92 Cs133 0.00 0.00 0.00 0.00 Ba138 1785 1736 144 1986 La139 24.67 22.86 2.33 24.64 Ce140 32.58 30.69 3.44 31.02 Pr141 2.25 2.06 0.26 2.00 Nd146 6.43 5.72 0.82 5.35 Sm147 0.65 0.42 0.10 0.50 Eu151 6.92 6.84 0.71 6.29 Gd157 1.14 0.92 0.13 0.94 Tb159 0.05 0.03 0.01 0.02 Pb208 22.45 22.99 2.29 22.02

300 Unit CAN CAN CAN CAN CAN CAN-silver CAN-silver CAN-silver CAN-silver Sample 0934 0934 0934 0934 0934 08CP21B 08CP21B 08CP21B 08CP21B mineral p p p p p pppp c/i/r c c c c c rrrr Line Numbers 91 92 93 94 95 815 816 817 818 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 7.13 7.13 7.39 7.45 7.45 7.64 7.85 8.05 7.71 Al2O3 Oxide Percents 24.90 25.14 24.95 24.08 23.90 22.92 22.94 23.98 24.24 SiO2 Oxide Percents 60.25 60.63 60.74 61.29 61.67 62.46 61.94 60.72 60.65 K2O Oxide Percents 0.98 1.03 0.95 1.29 1.33 2.16 1.91 1.13 1.16 FeO Oxide Percents 0.32 0.35 0.31 0.29 0.33 0.29 0.29 0.35 0.35 BaO Oxide Percents 0.17 0.16 0.17 0.19 0.16 0.35 0.30 0.31 0.22 CaO Oxide Percents 6.52 6.57 6.34 5.44 5.34 4.11 4.17 5.14 5.62 Oxide Totals 100.27 101.01 100.85 100.04 100.18 99.92 99.40 99.67 99.95

Na Formula Atoms 0.61 0.61 0.63 0.64 0.64 0.66 0.68 0.70 0.67 Al Formula Atoms 1.31 1.31 1.30 1.26 1.25 1.21 1.21 1.27 1.28 Si Formula Atoms 2.68 2.68 2.68 2.73 2.74 2.79 2.78 2.72 2.71 K Formula Atoms 0.06 0.06 0.05 0.07 0.08 0.12 0.11 0.06 0.07 Fe Formula Atoms 0.04 0.04 0.03 0.03 0.04 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.00 0.00 0.01 0.01 0.01 0.00 Ca Formula Atoms 0.31 0.31 0.30 0.26 0.25 0.20 0.20 0.25 0.27 Formula Totals 13.00 13.00 13.01 13.00 13.00 13.00 13.01 13.02 13.01 100*Ca/(Ca+Na) 33.57 33.75 32.15 28.75 28.34 22.93 22.72 26.08 28.71

An 31.67 31.75 30.41 26.59 26.14 20.06 20.22 24.41 26.81 Ab 62.68 62.33 64.17 65.90 66.09 67.43 68.77 69.19 66.59 Or 5.65 5.92 5.42 7.52 7.76 12.52 11.01 6.39 6.59

Grain Average 29.31 64.23 6.45

LA-ICP-MS (ppm) cc Si29 47812884.79 44072689.97 Mg25 90.94 95.56 Ca43 4.45 5.10 Ti47 224.88 181.25 Rb85 2.90 2.27 Sr88 414.46 428.24 Y89 1.02 0.99 Cs133 0.00 0.00 Ba138 1173 1162 La139 16.55 20.55 Ce140 26.39 29.51 Pr141 1.94 2.21 Nd146 5.96 6.03 Sm147 0.62 0.67 Eu151 5.27 5.51 Gd157 0.68 0.76 Tb159 0.03 0.05 Pb208 19.55 17.48

301 Unit CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral pp p p p pppp c/i/r cc c c c cccc Line Numbers 819 820 821 822 823 839 840 841 842 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 7.69 7.76 7.46 7.05 7.59 7.56 7.61 7.43 7.69 Al2O3 Oxide Percents 23.87 23.85 24.45 25.37 23.91 24.59 25.03 24.76 23.65 SiO2 Oxide Percents 60.57 60.74 59.90 58.85 61.21 60.35 60.17 60.04 60.87 K2O Oxide Percents 1.35 1.36 1.15 0.88 1.60 1.13 1.11 1.12 1.38 FeO Oxide Percents 0.26 0.32 0.36 0.32 0.36 0.30 0.34 0.28 0.29 BaO Oxide Percents 0.09 0.14 0.05 0.19 0.20 0.13 0.18 0.14 0.22 CaO Oxide Percents 5.39 5.40 6.07 6.78 5.26 5.67 6.18 6.25 5.03 Oxide Totals 99.23 99.57 99.46 99.44 100.12 99.73 100.61 100.02 99.14

Na Formula Atoms 0.67 0.68 0.65 0.62 0.66 0.66 0.66 0.64 0.67 Al Formula Atoms 1.27 1.26 1.30 1.35 1.26 1.30 1.31 1.31 1.26 Si Formula Atoms 2.73 2.73 2.69 2.65 2.73 2.70 2.68 2.69 2.74 K Formula Atoms 0.08 0.08 0.07 0.05 0.09 0.06 0.06 0.06 0.08 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.26 0.26 0.29 0.33 0.25 0.27 0.29 0.30 0.24 Formula Totals 13.01 13.02 13.02 13.01 13.01 13.01 13.02 13.01 13.01 100*Ca/(Ca+Na) 27.93 27.77 31.02 34.68 27.66 29.30 30.97 31.73 26.56

An 25.79 25.64 28.99 32.93 25.14 27.39 29.05 29.71 24.43 Ab 66.54 66.68 64.46 62.01 65.76 66.11 64.75 63.94 67.57 Or 7.67 7.68 6.55 5.06 9.10 6.49 6.19 6.35 7.99

Grain Average 25.56 66.38 8.06

LA-ICP-MS (ppm) rc Si29 41698783.65 39781249.68 Mg25 84.99 94.61 Ca43 3.82 4.23 Ti47 173.46 172.43 Rb85 4.20 4.61 Sr88 443.94 426.61 Y89 0.50 4.39 Cs133 0.01 0.02 Ba138 1587 960 La139 22.06 21.35 Ce140 29.96 35.97 Pr141 2.02 3.03 Nd146 5.40 11.20 Sm147 0.62 1.79 Eu151 6.55 5.48 Gd157 0.40 1.39 Tb159 0.02 0.17 Pb208 18.52 17.46

302 Unit CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral pp p p ppppp c/i/r rr r r rrrcc Line Numbers 843 844 845 846 859 860 861 862 863 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 8.07 8.27 8.32 8.42 7.81 8.12 8.00 7.64 7.36 Al2O3 Oxide Percents 22.64 22.97 22.45 23.21 23.04 22.98 22.82 23.63 24.57 SiO2 Oxide Percents 62.59 62.46 62.46 61.39 62.20 62.67 62.63 61.58 59.54 K2O Oxide Percents 1.94 1.65 1.72 1.48 1.92 1.53 1.82 1.67 1.14 FeO Oxide Percents 0.31 0.27 0.33 0.31 0.30 0.33 0.31 0.30 0.30 BaO Oxide Percents 0.33 0.17 0.11 0.27 0.45 0.27 0.32 0.00 0.00 CaO Oxide Percents 3.85 3.86 3.90 4.23 4.44 4.02 4.04 4.86 5.86 Oxide Totals 99.72 99.65 99.29 99.30 100.14 99.92 99.94 99.70 98.78

Na Formula Atoms 0.70 0.72 0.72 0.73 0.68 0.70 0.69 0.66 0.65 Al Formula Atoms 1.19 1.21 1.19 1.23 1.21 1.21 1.20 1.25 1.31 Si Formula Atoms 2.80 2.79 2.80 2.76 2.78 2.79 2.80 2.75 2.69 K Formula Atoms 0.11 0.09 0.10 0.08 0.11 0.09 0.10 0.10 0.07 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.01 0.00 0.00 0.00 0.01 0.00 0.01 0.00 0.00 Ca Formula Atoms 0.18 0.18 0.19 0.20 0.21 0.19 0.19 0.23 0.28 Formula Totals 13.01 13.01 13.01 13.03 13.01 13.00 13.00 13.00 13.01 100*Ca/(Ca+Na) 20.88 20.51 20.59 21.72 23.90 21.48 21.84 26.00 30.56

An 18.56 18.57 18.58 19.92 21.28 19.57 19.55 23.50 28.54 Ab 70.33 71.97 71.66 71.80 67.77 71.55 69.99 66.90 64.85 Or 11.11 9.46 9.76 8.28 10.95 8.88 10.45 9.60 6.61

Grain Average 23.28 68.52 8.21

LA-ICP-MS (ppm) c Si29 30451413.25 Mg25 99.33 Ca43 4.17 Ti47 197.82 Rb85 4.08 Sr88 355.89 Y89 0.91 Cs133 0.01 Ba138 1426 La139 23.38 Ce140 36.02 Pr141 2.36 Nd146 6.78 Sm147 0.72 Eu151 5.55 Gd157 0.63 Tb159 0.04 Pb208 27.04

303 Unit CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral p p p pppppp c/i/r c r r rrcccc Line Numbers 864 865 866 867 868 901 902 903 904 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 7.42 7.77 7.67 7.87 8.05 7.86 7.94 7.67 7.53 Al2O3 Oxide Percents 23.84 22.78 23.28 22.68 22.68 23.43 23.91 24.39 24.75 SiO2 Oxide Percents 60.72 62.57 62.03 61.95 62.34 61.54 61.47 59.53 60.09 K2O Oxide Percents 1.33 2.07 1.80 2.02 1.71 1.27 1.23 1.06 1.09 FeO Oxide Percents 0.30 0.32 0.31 0.32 0.29 0.33 0.34 0.32 0.29 BaO Oxide Percents 0.00 0.00 0.00 0.00 0.00 0.14 0.20 0.25 0.18 CaO Oxide Percents 5.63 4.09 4.54 3.94 4.01 4.79 5.04 5.81 5.97 Oxide Totals 99.23 99.64 99.63 98.78 99.08 99.36 100.13 99.03 99.91

Na Formula Atoms 0.65 0.67 0.66 0.69 0.70 0.68 0.69 0.67 0.65 Al Formula Atoms 1.26 1.20 1.23 1.21 1.20 1.24 1.26 1.30 1.31 Si Formula Atoms 2.73 2.80 2.77 2.79 2.80 2.76 2.74 2.69 2.69 K Formula Atoms 0.08 0.12 0.10 0.12 0.10 0.07 0.07 0.06 0.06 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.27 0.20 0.22 0.19 0.19 0.23 0.24 0.28 0.29 Formula Totals 13.00 13.00 13.00 13.01 13.00 13.00 13.01 13.02 13.01 100*Ca/(Ca+Na) 29.55 22.52 24.64 21.68 21.58 25.18 25.98 29.51 30.49

An 27.28 19.83 22.07 19.15 19.44 23.32 24.16 27.73 28.59 Ab 65.04 68.22 67.52 69.19 70.65 69.29 68.83 66.25 65.18 Or 7.68 11.95 10.41 11.66 9.90 7.38 7.01 6.02 6.23

Grain Average 22.02 68.17 9.81

LA-ICP-MS (ppm) rcr Si29 36898977.00 ######### ######### Mg25 78.53 84.50 74.14 Ca43 2.90 3.80 3.20 Ti47 179.37 166.64 163.40 Rb85 6.09 3.30 5.09 Sr88 370.76 359.95 373.27 Y89 0.42 0.46 0.38 Cs133 0.03 0.01 0.00 Ba138 1871 1221 1555 La139 20.78 16.13 19.56 Ce140 30.07 26.19 29.36 Pr141 1.83 1.68 1.80 Nd146 4.80 4.57 4.55 Sm147 0.46 0.52 0.46 Eu151 5.57 5.11 5.02 Gd157 0.36 0.45 0.31 Tb159 0.02 0.02 0.02 Pb208 21.32 19.91 21.94

304 Unit DRF DRF DRF DRF DRF DRF DRF DRF DRF DRF Sample 08CP09 08CP09 08CP09 08CP09 08CP09 08CP09 mineral pp p p p p pppp c/i/r ri c i r r iicc Line Numbers 295 296 297 298 299 301 302 303 304 305 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 8.87 8.75 8.88 9.03 8.91 8.67 8.41 8.80 8.78 8.74 Al2O3 Oxide Percents 22.62 23.18 23.00 22.68 22.58 22.86 23.14 23.40 23.14 23.15 SiO2 Oxide Percents 62.18 61.52 61.15 62.06 63.09 61.54 61.19 61.68 61.68 61.31 K2O Oxide Percents 1.06 1.24 1.13 0.82 1.14 1.33 1.30 1.16 1.01 0.89 FeO Oxide Percents 0.35 0.35 0.28 0.32 0.35 0.36 0.27 0.32 0.31 0.32 BaO Oxide Percents 0.15 0.17 0.14 0.15 0.24 0.15 0.10 0.23 0.23 0.08 CaO Oxide Percents 4.58 4.87 4.93 4.41 4.34 4.71 4.90 4.77 5.04 5.12 Oxide Totals 99.80 100.08 99.51 99.46 100.66 99.63 99.30 100.36 100.19 99.61

Na Formula Atoms 0.77 0.76 0.77 0.78 0.77 0.76 0.73 0.76 0.76 0.76 Al Formula Atoms 1.19 1.22 1.22 1.20 1.18 1.21 1.23 1.23 1.22 1.22 Si Formula Atoms 2.78 2.75 2.75 2.78 2.80 2.76 2.75 2.75 2.75 2.75 K Formula Atoms 0.06 0.07 0.06 0.05 0.06 0.08 0.07 0.07 0.06 0.05 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Ca Formula Atoms 0.22 0.23 0.24 0.21 0.21 0.23 0.24 0.23 0.24 0.25 Formula Totals 13.04 13.05 13.06 13.04 13.03 13.05 13.04 13.05 13.05 13.04 100*Ca/(Ca+Na) 22.20 23.55 23.46 21.23 21.22 23.09 24.35 23.06 24.07 24.47

An 20.92 21.98 22.05 20.28 19.90 21.42 22.61 21.61 22.76 23.28 Ab 73.31 71.36 71.95 75.22 73.87 71.36 70.24 72.11 71.81 71.87 Or 5.78 6.67 6.01 4.50 6.23 7.22 7.15 6.28 5.43 4.84

Grain Average 21.02 73.14 5.84

LA-ICP-MS (ppm) rcc Si29 37918184.50 37235507.58 43792528.59 Mg25 47.79 52.49 51.33 Ca43 2.78 3.04 2.90 Ti47 81.09 69.33 66.42 Rb85 6.04 3.15 3.10 Sr88 199.41 203.18 185.69 Y89 0.79 0.27 0.26 Cs133 0.08 0.00 0.00 Ba138 1193 994 965 La139 16.84 15.15 15.05 Ce140 25.11 21.47 22.56 Pr141 1.64 1.35 1.42 Nd146 4.33 3.80 3.56 Sm147 0.40 0.36 0.38 Eu151 2.43 2.41 2.36 Gd157 0.27 0.20 0.21 Tb159 0.04 0.02 0.01 Pb208 20.92 17.91 19.80

305

APPENDIX K

RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF SANADINE FROM THE EUBM

Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral s s sssssss c/i/r r c r r iiiii Line Numbers 33 34 37 38 39 40 41 42 44 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.07 5.24 5.60 5.71 5.34 5.08 5.06 5.01 5.02 Al2O3 Oxide Percents 19.88 19.80 19.90 20.18 19.82 19.87 19.61 19.71 19.45 SiO2 Oxide Percents 64.55 64.81 64.01 64.31 64.21 64.29 65.15 64.82 65.08 K2O Oxide Percents 8.03 7.78 7.29 6.71 7.58 7.88 8.40 8.40 8.30 FeO Oxide Percents 0.21 0.19 0.17 0.22 0.20 0.22 0.20 0.18 0.18 BaO Oxide Percents 1.70 1.73 1.71 1.58 1.68 1.83 1.67 1.50 1.46 CaO Oxide Percents 0.73 0.78 1.00 1.28 0.92 0.82 0.60 0.70 0.59 Oxide Totals 100.16 100.33 99.68 99.99 99.74 100.00 100.70 100.32 100.07

Na Formula Atoms 0.45 0.46 0.50 0.50 0.47 0.45 0.44 0.44 0.44 Al Formula Atoms 1.07 1.06 1.07 1.08 1.07 1.07 1.05 1.05 1.04 Si Formula Atoms 2.94 2.94 2.92 2.92 2.93 2.93 2.95 2.94 2.96 K Formula Atoms 0.47 0.45 0.42 0.39 0.44 0.46 0.49 0.49 0.48 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.03 Ca Formula Atoms 0.04 0.04 0.05 0.06 0.04 0.04 0.03 0.03 0.03 Formula Totals 12.99 12.99 13.00 12.99 12.99 12.99 12.99 12.99 12.98 100*Ca/(Ca+Na) 7.37 7.60 8.99 11.04 8.68 8.23 6.16 7.16 6.12

An 3.75 3.99 5.05 6.54 4.69 4.25 3.04 3.53 3.03 Ab 47.11 48.56 51.15 52.71 49.29 47.36 46.35 45.84 46.43 Or 49.14 47.45 43.79 40.76 46.03 48.39 50.61 50.62 50.54

Grain Average 3.87 47.84 48.29

LA-ICP-MS (ppm) r c Si29 45079156.67 38754832.64 Mg25 25.59 94.56 Ca43 0.63 3.01 Ti47 207.74 170.54 Rb85 187.48 12.39 Sr88 119.00 374.21 Y89 1.28 0.56 Cs133 0.22 0.03 Ba138 6571.58 1821.28 La139 8.19 22.20 Ce140 11.17 31.41 Pr141 0.65 1.89 Nd146 1.81 5.12 Sm147 0.22 0.43 Eu151 2.77 5.83 Gd157 0.29 0.34 Tb159 0.03 0.02 Pb208 51.82 25.44

307 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral ssssssssss c/i/r ccccciiiii Line Numbers 45 46 47 48 49 50 51 52 53 54 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.02 4.92 5.15 5.25 5.06 4.92 4.94 4.69 4.98 5.16 Al2O3 Oxide Percents 19.77 19.54 19.79 19.72 19.77 19.58 19.61 19.37 19.79 20.00 SiO2 Oxide Percents 65.55 64.73 65.77 65.56 64.53 64.50 65.01 64.99 63.58 64.13 K2O Oxide Percents 8.33 8.25 8.37 8.20 8.20 8.43 8.40 8.55 8.28 7.93 FeO Oxide Percents 0.21 0.17 0.18 0.21 0.21 0.18 0.22 0.17 0.20 0.20 BaO Oxide Percents 1.42 1.39 1.44 1.36 1.56 1.59 1.59 1.70 1.88 1.84 CaO Oxide Percents 0.69 0.71 0.63 0.71 0.60 0.68 0.65 0.64 0.76 0.73 Oxide Totals 100.99 99.72 101.33 101.01 99.92 99.90 100.41 100.09 99.48 99.97

Na Formula Atoms 0.44 0.44 0.45 0.46 0.45 0.44 0.43 0.41 0.44 0.46 Al Formula Atoms 1.05 1.05 1.05 1.05 1.06 1.05 1.05 1.04 1.07 1.08 Si Formula Atoms 2.95 2.95 2.95 2.95 2.94 2.94 2.95 2.96 2.92 2.93 K Formula Atoms 0.48 0.48 0.48 0.47 0.48 0.49 0.49 0.50 0.49 0.46 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.02 0.03 0.02 0.03 0.03 0.03 0.03 0.03 0.03 Ca Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.04 0.04 Formula Totals 12.98 12.98 12.99 12.99 12.99 12.99 12.99 12.98 13.01 13.00 100*Ca/(Ca+Na) 7.08 7.40 6.33 6.95 6.17 7.11 6.75 6.97 7.73 7.23

An 3.52 3.66 3.16 3.55 3.08 3.47 3.30 3.29 3.85 3.73 Ab 46.14 45.82 46.81 47.59 46.90 45.38 45.64 43.98 45.93 47.85 Or 50.34 50.52 50.03 48.86 50.02 51.14 51.05 52.73 50.22 48.41

Grain Average

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

308 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral sssss sssss c/i/r iirrr rriii Line Numbers 55 56 57 58 59 60 61 62 63 64 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.10 5.21 5.29 5.25 5.68 5.33 5.46 5.07 5.04 5.17 Al2O3 Oxide Percents 19.83 19.26 19.65 20.03 20.15 20.04 19.96 19.42 19.49 19.40 SiO2 Oxide Percents 64.00 65.00 64.63 64.70 65.41 64.68 64.88 64.85 65.60 65.07 K2O Oxide Percents 7.89 8.09 7.92 7.61 7.63 7.63 7.36 8.32 8.11 7.93 FeO Oxide Percents 0.19 0.17 0.19 0.20 0.19 0.19 0.21 0.16 0.22 0.21 BaO Oxide Percents 1.89 1.51 1.65 1.71 1.23 1.57 1.80 1.36 1.48 1.46 CaO Oxide Percents 0.82 0.62 0.69 0.90 1.00 0.86 0.87 0.67 0.63 0.73 Oxide Totals 99.72 99.86 100.03 100.40 101.28 100.30 100.55 99.86 100.58 99.96

Na Formula Atoms 0.45 0.46 0.47 0.46 0.49 0.47 0.48 0.45 0.44 0.46 Al Formula Atoms 1.07 1.03 1.05 1.07 1.06 1.07 1.06 1.04 1.04 1.04 Si Formula Atoms 2.93 2.96 2.94 2.93 2.93 2.93 2.93 2.95 2.96 2.96 K Formula Atoms 0.46 0.47 0.46 0.44 0.44 0.44 0.42 0.48 0.47 0.46 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.02 0.03 0.03 0.02 0.03 0.03 Ca Formula Atoms 0.04 0.03 0.03 0.04 0.05 0.04 0.04 0.03 0.03 0.04 Formula Totals 12.99 12.99 12.99 12.98 13.00 12.99 12.98 12.99 12.97 12.98 100*Ca/(Ca+Na) 8.19 6.16 6.75 8.67 8.83 8.19 8.10 6.77 6.49 7.21

An 4.23 3.14 3.52 4.63 4.89 4.39 4.46 3.37 3.27 3.72 Ab 47.44 47.89 48.62 48.83 50.49 49.23 50.63 46.46 47.01 47.89 Or 48.33 48.97 47.86 46.54 44.62 46.38 44.91 50.16 49.73 48.39

Grain Average

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

309 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral sssssss s s c/i/r iccci i i i r Line Numbers 65 66 67 68 69 70 71 72 73 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 4.96 5.11 4.98 4.97 4.97 5.01 4.92 4.77 4.77 Al2O3 Oxide Percents 19.53 19.81 19.59 19.59 19.50 19.37 19.49 19.38 19.42 SiO2 Oxide Percents 65.61 65.44 64.65 64.79 64.07 65.11 64.81 65.38 65.89 K2O Oxide Percents 8.17 8.30 8.25 8.23 8.56 8.23 8.38 8.69 8.66 FeO Oxide Percents 0.19 0.20 0.20 0.20 0.24 0.19 0.20 0.25 0.20 BaO Oxide Percents 1.54 1.55 1.63 1.56 1.50 1.44 1.42 1.70 1.67 CaO Oxide Percents 0.58 0.67 0.56 0.56 0.56 0.72 0.68 0.54 0.48 Oxide Totals 100.59 101.08 99.85 99.89 99.41 100.06 99.90 100.71 101.09

Na Formula Atoms 0.43 0.45 0.44 0.44 0.44 0.44 0.43 0.42 0.42 Al Formula Atoms 1.04 1.05 1.05 1.05 1.06 1.04 1.05 1.03 1.03 Si Formula Atoms 2.96 2.95 2.95 2.95 2.94 2.96 2.95 2.96 2.97 K Formula Atoms 0.47 0.48 0.48 0.48 0.50 0.48 0.49 0.50 0.50 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.03 Ca Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.04 0.03 0.03 0.02 Formula Totals 12.97 12.99 12.99 12.98 13.00 12.98 12.99 12.98 12.97 100*Ca/(Ca+Na) 6.05 6.75 5.86 5.83 5.91 7.36 7.12 5.87 5.30

An 3.00 3.38 2.89 2.88 2.86 3.68 3.49 2.75 2.49 Ab 46.57 46.72 46.48 46.51 45.53 46.30 45.51 44.20 44.43 Or 50.44 49.90 50.63 50.61 51.62 50.02 51.00 53.05 53.08

Grain Average

LA-ICP-MS (ppm) ri Si29 38972805.55 36962933.77 Mg25 30.32 20.34 Ca43 0.95 0.92 Ti47 298.32 236.96 Rb85 130.45 100.98 Sr88 266.61 353.39 Y89 2.86 1.08 Cs133 0.24 0.12 Ba138 9269.86 11455.04 La139 11.91 10.59 Ce140 12.96 9.98 Pr141 0.80 0.48 Nd146 2.95 1.17 Sm147 0.45 0.12 Eu151 5.29 6.37 Gd157 0.62 0.28 Tb159 0.07 0.01 Pb208 39.87 32.66

310 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral s ssss s s ss c/i/r r rrrc c c rr Line Numbers 74 101 102 103 104 105 106 107 108 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.29 5.43 5.77 5.30 4.67 4.75 4.82 5.61 5.46 Al2O3 Oxide Percents 20.05 19.84 19.73 19.64 19.46 19.22 19.26 19.98 19.85 SiO2 Oxide Percents 64.80 65.14 64.70 64.15 63.88 64.95 65.50 65.16 65.01 K2O Oxide Percents 7.93 7.62 7.34 8.08 8.42 8.76 8.73 7.11 7.54 FeO Oxide Percents 0.21 0.20 0.20 0.18 0.19 0.21 0.18 0.19 0.20 BaO Oxide Percents 1.15 1.38 1.17 1.61 1.60 1.52 1.65 0.86 1.38 CaO Oxide Percents 0.87 0.90 0.97 0.81 0.56 0.52 0.53 1.04 0.90 Oxide Totals 100.30 100.53 99.87 99.78 98.77 99.92 100.68 99.94 100.35

Na Formula Atoms 0.46 0.48 0.51 0.47 0.42 0.42 0.42 0.49 0.48 Al Formula Atoms 1.07 1.06 1.06 1.06 1.06 1.03 1.03 1.06 1.06 Si Formula Atoms 2.93 2.94 2.94 2.93 2.95 2.96 2.97 2.94 2.94 K Formula Atoms 0.46 0.44 0.43 0.47 0.50 0.51 0.50 0.41 0.44 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.02 0.02 0.02 0.03 0.03 0.03 0.03 0.02 0.02 Ca Formula Atoms 0.04 0.04 0.05 0.04 0.03 0.03 0.03 0.05 0.04 Formula Totals 12.99 12.99 13.00 13.01 12.98 12.99 12.98 12.98 12.99 100*Ca/(Ca+Na) 8.33 8.36 8.51 7.76 6.20 5.67 5.78 9.33 8.37

An 4.37 4.53 4.82 4.03 2.93 2.64 2.72 5.31 4.56 Ab 48.11 49.65 51.82 47.91 44.38 44.00 44.38 51.64 49.98 Or 47.51 45.82 43.36 48.06 52.69 53.35 52.89 43.04 45.46

Grain Average 3.68 3.61 47.19 47.02 49.13 49.36

LA-ICP-MS (ppm) crc Si29 34896915.13 43953704.55 46672685.70 Mg25 23.30 41.27 123.26 Ca43 0.82 0.66 0.66 Ti47 229.01 217.20 286.27 Rb85 97.53 167.50 125.42 Sr88 313.00 130.21 219.83 Y89 0.93 2.09 7.31 Cs133 0.08 0.21 0.24 Ba138 9741.59 6954.95 7948.57 La139 9.65 9.10 13.49 Ce140 8.93 9.30 18.74 Pr141 0.44 0.86 2.12 Nd146 1.01 3.75 7.90 Sm147 0.06 0.45 1.83 Eu151 5.52 3.13 4.01 Gd157 0.19 0.70 1.54 Tb159 0.01 0.07 0.23 Pb208 29.16 46.12 30.54

311 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 07CP05 mineral ssssssssss c/i/r iiiccciiii Line Numbers 109 110 111 112 113 114 116 124 125 126 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.31 5.26 5.36 5.26 5.09 5.15 4.76 4.88 5.00 5.18 Al2O3 Oxide Percents 19.98 19.60 19.85 19.82 19.64 19.75 18.84 19.58 19.82 19.87 SiO2 Oxide Percents 64.25 63.92 63.84 64.31 64.50 65.54 65.97 65.27 64.46 64.63 K2O Oxide Percents 7.83 7.77 7.62 7.77 7.86 7.65 9.04 8.58 7.94 8.05 FeO Oxide Percents 0.17 0.21 0.19 0.18 0.19 0.22 0.17 0.19 0.19 0.18 BaO Oxide Percents 1.78 1.77 1.76 1.74 1.86 1.70 1.13 1.60 1.75 1.72 CaO Oxide Percents 0.90 0.77 0.90 0.89 0.80 0.84 0.27 0.54 0.73 0.75 Oxide Totals 100.23 99.30 99.53 99.97 99.92 100.85 100.18 100.63 99.88 100.38

Na Formula Atoms 0.47 0.47 0.48 0.46 0.45 0.45 0.42 0.43 0.44 0.46 Al Formula Atoms 1.07 1.06 1.07 1.06 1.06 1.05 1.01 1.04 1.06 1.06 Si Formula Atoms 2.92 2.93 2.92 2.93 2.94 2.95 2.99 2.95 2.94 2.93 K Formula Atoms 0.45 0.46 0.45 0.45 0.46 0.44 0.52 0.50 0.46 0.47 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.03 0.02 0.03 0.03 0.03 Ca Formula Atoms 0.04 0.04 0.04 0.04 0.04 0.04 0.01 0.03 0.04 0.04 Formula Totals 13.00 13.00 13.00 12.99 12.98 12.97 12.98 12.98 12.98 12.99 100*Ca/(Ca+Na) 8.57 7.53 8.50 8.52 7.97 8.27 3.08 5.78 7.47 7.40

An 4.54 3.96 4.58 4.51 4.12 4.36 1.39 2.77 3.80 3.80 Ab 48.47 48.69 49.30 48.42 47.55 48.36 43.84 45.10 47.04 47.54 Or 46.99 47.35 46.12 47.06 48.34 47.29 54.76 52.13 49.16 48.66

Grain Average

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

312 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP05 07CP05 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 07CP04 mineral s s sssssss c/i/r rr ricrrcr Line Numbers 127 128 138 139 140 141 148 149 150 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.18 5.53 5.10 5.05 5.15 4.97 5.42 5.24 5.20 Al2O3 Oxide Percents 19.89 20.03 19.07 19.99 19.72 19.15 19.95 19.65 20.08 SiO2 Oxide Percents 65.10 65.57 66.24 64.02 64.11 66.37 64.79 64.79 64.69 K2O Oxide Percents 7.88 7.42 8.94 8.08 7.78 8.99 7.78 7.89 8.36 FeO Oxide Percents 0.18 0.20 0.24 0.20 0.19 0.10 0.19 0.23 0.17 BaO Oxide Percents 1.44 1.18 0.17 1.77 1.71 0.21 1.74 1.81 1.69 CaO Oxide Percents 0.80 1.00 0.45 0.84 0.86 0.52 0.77 0.78 0.68 Oxide Totals 100.46 100.94 100.20 99.95 99.53 100.29 100.66 100.39 100.88

Na Formula Atoms 0.45 0.48 0.45 0.45 0.46 0.43 0.48 0.46 0.46 Al Formula Atoms 1.06 1.06 1.01 1.08 1.06 1.02 1.06 1.05 1.07 Si Formula Atoms 2.94 2.94 2.98 2.92 2.93 2.99 2.93 2.94 2.93 K Formula Atoms 0.45 0.42 0.51 0.47 0.45 0.52 0.45 0.46 0.48 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.00 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.02 0.00 0.03 0.03 0.00 0.03 0.03 0.03 Ca Formula Atoms 0.04 0.05 0.02 0.04 0.04 0.03 0.04 0.04 0.03 Formula Totals 12.98 12.98 12.99 13.00 12.99 12.98 13.00 12.99 13.01 100*Ca/(Ca+Na) 7.83 9.06 4.64 8.38 8.42 5.46 7.31 7.65 6.75

An 4.08 5.02 2.21 4.27 4.41 2.57 3.90 3.99 3.40 Ab 47.95 50.44 45.42 46.64 47.94 44.47 49.42 48.21 46.96 Or 47.97 44.54 52.37 49.09 47.65 52.96 46.68 47.80 49.64

Grain Average 4.06 3.36 3.76 48.17 46.12 48.20 47.78 50.52 48.04

LA-ICP-MS (ppm) rc Si29 40010181.05 42521694.84 Mg25 44.22 44.47 Ca43 0.85 0.92 Ti47 228.26 298.80 Rb85 147.50 142.50 Sr88 195.11 286.14 Y89 2.22 4.89 Cs133 0.18 0.30 Ba138 8713.65 8093.59 La139 12.08 12.22 Ce140 11.48 12.70 Pr141 0.86 1.22 Nd146 2.06 4.27 Sm147 0.40 1.28 Eu151 4.43 5.15 Gd157 0.68 1.14 Tb159 0.06 0.13 Pb208 45.65 40.61

313 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP04 07CP04 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 mineral ssss sssss c/i/r rccr riiii Line Numbers 158 159 163 164 201 202 203 204 205 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.56 4.99 5.31 4.87 5.71 5.14 5.21 5.25 5.14 Al2O3 Oxide Percents 19.81 19.71 20.08 19.60 19.87 20.01 19.85 19.93 19.92 SiO2 Oxide Percents 64.65 63.83 65.01 63.89 65.31 64.30 64.55 64.42 64.46 K2O Oxide Percents 7.61 8.02 7.63 8.12 7.37 7.54 7.79 7.88 7.81 FeO Oxide Percents 0.21 0.19 0.23 0.18 0.23 0.22 0.22 0.29 0.25 BaO Oxide Percents 1.31 2.10 1.50 1.73 1.12 1.81 1.99 1.99 2.13 CaO Oxide Percents 0.91 0.68 0.89 0.69 0.91 0.86 0.81 0.79 0.77 Oxide Totals 100.05 99.53 100.64 99.07 100.52 99.87 100.41 100.56 100.48

Na Formula Atoms 0.49 0.44 0.46 0.43 0.50 0.45 0.46 0.46 0.45 Al Formula Atoms 1.06 1.07 1.07 1.06 1.05 1.07 1.06 1.07 1.07 Si Formula Atoms 2.93 2.93 2.93 2.94 2.94 2.93 2.93 2.93 2.93 K Formula Atoms 0.44 0.47 0.44 0.48 0.42 0.44 0.45 0.46 0.45 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.02 0.04 0.03 0.03 0.02 0.03 0.04 0.04 0.04 Ca Formula Atoms 0.04 0.03 0.04 0.03 0.04 0.04 0.04 0.04 0.04 Formula Totals 13.00 12.99 12.98 12.98 12.99 12.98 12.99 13.00 12.99 100*Ca/(Ca+Na) 8.27 7.02 8.48 7.22 8.12 8.46 7.90 7.70 7.64

An 4.53 3.54 4.54 3.58 4.56 4.49 4.14 4.03 3.98 Ab 50.26 46.88 49.06 45.98 51.62 48.57 48.31 48.29 48.04 Or 45.21 49.58 46.40 50.45 43.82 46.94 47.55 47.68 47.99

Grain Average 4.04 4.06 48.57 47.52 47.39 48.42

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

314 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 mineral ssssssssss c/i/r iccccccccc Line Numbers 206 207 208 209 210 211 212 213 214 215 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.30 5.00 5.23 4.94 5.14 5.27 5.03 5.07 4.99 5.27 Al2O3 Oxide Percents 20.11 20.17 19.87 19.93 19.98 19.91 19.80 19.66 19.84 19.69 SiO2 Oxide Percents 64.21 64.50 64.64 64.66 64.46 64.29 64.25 64.20 64.26 64.25 K2O Oxide Percents 7.78 7.67 7.64 8.22 7.73 7.86 7.67 7.93 7.89 7.84 FeO Oxide Percents 0.28 0.24 0.20 0.16 0.20 0.18 0.21 0.20 0.21 0.18 BaO Oxide Percents 2.06 1.97 1.98 1.95 1.95 1.97 1.93 1.94 2.07 1.97 CaO Oxide Percents 0.83 0.92 0.82 0.77 0.82 0.84 0.80 0.78 0.79 0.81 Oxide Totals 100.57 100.46 100.39 100.65 100.27 100.32 99.69 99.79 100.05 100.02

Na Formula Atoms 0.47 0.44 0.46 0.43 0.45 0.47 0.45 0.45 0.44 0.47 Al Formula Atoms 1.08 1.08 1.06 1.07 1.07 1.07 1.07 1.06 1.07 1.06 Si Formula Atoms 2.92 2.93 2.94 2.93 2.93 2.93 2.94 2.94 2.93 2.93 K Formula Atoms 0.45 0.44 0.44 0.48 0.45 0.46 0.45 0.46 0.46 0.46 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.04 0.03 0.04 0.03 0.03 0.04 0.03 0.03 0.04 0.04 Ca Formula Atoms 0.04 0.04 0.04 0.04 0.04 0.04 0.04 0.04 0.04 0.04 Formula Totals 13.00 12.98 12.98 12.99 12.98 13.00 12.98 12.99 12.98 13.00 100*Ca/(Ca+Na) 7.98 9.22 7.94 7.96 8.12 8.12 8.04 7.80 8.06 7.80

An 4.22 4.81 4.22 3.97 4.25 4.27 4.18 4.00 4.12 4.10 Ab 48.70 47.36 48.85 45.86 48.13 48.31 47.82 47.33 46.98 48.47 Or 47.07 47.83 46.93 50.18 47.62 47.42 48.00 48.67 48.90 47.43

Grain Average

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

315 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 07CP03 mineral sssssssss c/i/r iiiiirrrr Line Numbers 216 217 218 220 221 222 223 224 225 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.50 5.12 5.17 5.36 5.03 5.18 4.75 5.39 4.95 Al2O3 Oxide Percents 19.95 19.90 19.85 19.93 19.79 19.64 18.43 19.60 19.65 SiO2 Oxide Percents 64.39 63.57 63.96 64.09 64.27 64.66 66.27 64.84 64.13 K2O Oxide Percents 7.85 7.65 7.78 7.83 7.66 7.66 9.22 7.66 7.86 FeO Oxide Percents 0.18 0.23 0.21 0.20 0.21 0.21 0.24 0.18 0.20 BaO Oxide Percents 1.82 1.96 1.88 1.79 1.86 1.62 0.11 1.11 2.00 CaO Oxide Percents 0.85 0.83 0.79 0.84 0.73 0.84 0.27 0.97 0.66 Oxide Totals 100.53 99.25 99.63 100.03 99.56 99.81 99.29 99.75 99.44

Na Formula Atoms 0.48 0.46 0.46 0.47 0.45 0.46 0.42 0.47 0.44 Al Formula Atoms 1.07 1.08 1.07 1.07 1.07 1.05 0.99 1.05 1.06 Si Formula Atoms 2.92 2.92 2.93 2.92 2.94 2.94 3.01 2.95 2.94 K Formula Atoms 0.45 0.45 0.45 0.46 0.45 0.44 0.53 0.44 0.46 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.04 0.03 0.03 0.03 0.03 0.00 0.02 0.04 Ca Formula Atoms 0.04 0.04 0.04 0.04 0.04 0.04 0.01 0.05 0.03 Formula Totals 13.01 12.99 12.99 13.01 12.97 12.98 12.97 12.99 12.98 100*Ca/(Ca+Na) 7.87 8.17 7.75 7.93 7.46 8.22 3.05 9.07 6.91

An 4.22 4.30 4.05 4.21 3.87 4.34 1.37 4.90 3.50 Ab 49.39 48.29 48.22 48.86 48.03 48.48 43.33 49.15 47.18 Or 46.40 47.42 47.73 46.93 48.10 47.18 55.31 45.95 49.31

Grain Average 4.09 48.06 47.85

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

316 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC TSC Sample 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 mineral ssssssssss c/i/r riccirrcrc Line Numbers 235 236 237 238 239 240 241 242 243 244 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.41 5.06 5.12 5.18 5.18 5.58 5.11 4.73 5.54 5.11 Al2O3 Oxide Percents 19.78 19.57 19.81 19.95 19.72 19.93 19.80 19.79 20.09 19.64 SiO2 Oxide Percents 64.38 64.41 64.01 64.61 64.57 65.59 64.66 64.84 64.10 64.51 K2O Oxide Percents 7.73 7.65 7.86 7.55 7.51 7.34 8.06 8.14 7.54 8.14 FeO Oxide Percents 0.19 0.18 0.21 0.22 0.19 0.21 0.21 0.19 0.20 0.17 BaO Oxide Percents 1.54 1.90 1.84 1.85 1.85 1.12 1.74 1.72 1.45 1.77 CaO Oxide Percents 0.73 0.76 0.87 0.85 0.83 1.00 0.73 0.69 0.99 0.77 Oxide Totals 99.76 99.53 99.71 100.22 99.85 100.77 100.31 100.09 99.91 100.12

Na Formula Atoms 0.48 0.45 0.45 0.46 0.46 0.49 0.45 0.42 0.49 0.45 Al Formula Atoms 1.06 1.06 1.07 1.07 1.06 1.05 1.06 1.06 1.08 1.05 Si Formula Atoms 2.94 2.95 2.93 2.93 2.94 2.94 2.94 2.95 2.92 2.94 K Formula Atoms 0.45 0.45 0.46 0.44 0.44 0.42 0.47 0.47 0.44 0.47 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.02 0.03 0.03 0.03 0.03 Ca Formula Atoms 0.04 0.04 0.04 0.04 0.04 0.05 0.04 0.03 0.05 0.04 Formula Totals 13.00 12.97 12.99 12.98 12.98 12.98 12.99 12.97 13.01 13.00 100*Ca/(Ca+Na) 6.95 7.66 8.55 8.34 8.12 9.01 7.29 7.44 9.01 7.69

An 3.71 3.99 4.45 4.44 4.32 5.04 3.72 3.63 4.97 3.91 Ab 49.63 48.10 47.55 48.80 48.96 50.90 47.22 45.21 50.15 46.94 Or 46.66 47.91 48.00 46.76 46.71 44.06 49.06 51.15 44.89 49.15

Grain Average 4.16 48.30 47.54

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

317 Unit TSC TSC TSC TSC TSC TSC TSC TSC TSC CAN Sample 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 07CP06 0934 mineral sssssssss s c/i/r crrcrcrrc r Line Numbers 245 246 247 248 249 250 251 252 253 32 Date 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009 2/11/2009

Na2O Oxide Percents 5.07 5.19 5.35 5.06 5.72 5.37 5.02 4.88 5.35 5.20 Al2O3 Oxide Percents 19.60 19.69 19.86 19.73 19.91 19.63 19.58 19.68 19.62 20.04 SiO2 Oxide Percents 65.12 64.64 64.79 64.91 65.30 65.24 65.16 64.68 64.64 64.97 K2O Oxide Percents 7.99 7.80 7.56 8.11 7.48 7.87 8.42 8.50 8.22 7.91 FeO Oxide Percents 0.18 0.22 0.19 0.21 0.19 0.21 0.26 0.22 0.17 0.18 BaO Oxide Percents 1.67 1.63 1.54 1.64 1.50 1.09 1.53 1.80 1.21 1.78 CaO Oxide Percents 0.70 0.76 0.75 0.62 0.90 0.89 0.63 0.65 0.81 0.82 Oxide Totals 100.33 99.92 100.05 100.28 101.01 100.31 100.59 100.40 100.02 100.89

Na Formula Atoms 0.45 0.46 0.47 0.45 0.50 0.47 0.44 0.43 0.47 0.46 Al Formula Atoms 1.05 1.06 1.06 1.06 1.06 1.05 1.04 1.05 1.05 1.07 Si Formula Atoms 2.95 2.94 2.94 2.95 2.94 2.95 2.95 2.94 2.94 2.93 K Formula Atoms 0.46 0.45 0.44 0.47 0.43 0.45 0.49 0.49 0.48 0.46 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.02 0.03 0.03 0.02 0.03 Ca Formula Atoms 0.03 0.04 0.04 0.03 0.04 0.04 0.03 0.03 0.04 0.04 Formula Totals 12.98 12.98 12.98 12.98 13.00 12.99 12.99 12.99 13.01 12.99 100*Ca/(Ca+Na) 7.09 7.45 7.22 6.35 8.02 8.41 6.47 6.90 7.76 8.04

An 3.61 3.89 3.88 3.20 4.48 4.46 3.18 3.34 4.01 4.19 Ab 47.30 48.33 49.81 47.11 51.37 48.61 46.02 45.03 47.73 47.89 Or 49.09 47.78 46.31 49.69 44.15 46.93 50.80 51.64 48.26 47.92

Grain Average 3.54 3.90 48.46 47.75 48.00 48.35

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

318 Unit CAN CAN CAN CAN CAN CAN CAN CF/TSC CF/TSC Sample 0934 0934 0934 0934 0934 0934 0934 08CP21B 08CP21B mineral s s s ssss s s c/i/r c r c crrr c c Line Numbers 33 34 35 193 194 195 196 787 788 Date 7/13/2009 7/13/2009

Na2O Oxide Percents 5.34 5.20 5.33 5.49 5.19 5.34 5.21 5.18 5.47 Al2O3 Oxide Percents 19.95 20.09 19.89 20.01 19.93 20.02 19.66 19.79 19.98 SiO2 Oxide Percents 65.31 65.11 64.57 64.17 64.67 64.46 65.11 64.73 64.63 K2O Oxide Percents 7.62 7.81 7.62 7.58 8.02 7.81 8.05 8.29 7.97 FeO Oxide Percents 0.20 0.18 0.20 0.25 0.20 0.17 0.20 0.17 0.20 BaO Oxide Percents 1.70 1.75 1.63 1.84 1.70 1.85 1.52 1.19 1.21 CaO Oxide Percents 0.87 0.78 0.74 0.95 0.83 0.84 0.72 0.77 0.89 Oxide Totals 100.99 100.92 99.98 100.29 100.55 100.50 100.48 100.13 100.34

Na Formula Atoms 0.47 0.45 0.47 0.48 0.46 0.47 0.46 0.46 0.48 Al Formula Atoms 1.06 1.07 1.06 1.07 1.06 1.07 1.05 1.06 1.07 Si Formula Atoms 2.93 2.93 2.93 2.91 2.93 2.92 2.94 2.94 2.93 K Formula Atoms 0.44 0.45 0.44 0.44 0.46 0.45 0.46 0.48 0.46 Fe Formula Atoms 0.02 0.02 0.02 0.03 0.02 0.02 0.02 0.01 0.01 Ba Formula Atoms 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.02 0.02 Ca Formula Atoms 0.04 0.04 0.04 0.05 0.04 0.04 0.03 0.04 0.04 Formula Totals 12.99 12.99 12.99 13.01 13.00 13.00 12.99 13.00 13.01 100*Ca/(Ca+Na) 8.26 7.64 7.10 8.72 8.13 8.00 7.06 7.69 8.22

An 4.44 4.00 3.79 4.77 4.20 4.25 3.63 3.90 4.37 Ab 49.29 48.32 49.57 49.88 47.50 48.80 47.80 46.82 48.78 Or 46.27 47.69 46.64 45.36 48.30 46.95 48.57 49.28 46.85

Grain Average 4.10 4.21 48.77 48.50 47.13 47.29

LA-ICP-MS (ppm) rc Si29 66241895.97 58045475.57 Mg25 57.36 315.18 Ca43 1.33 1.58 Ti47 223.36 308.96 Rb85 51.63 51.51 Sr88 381.55 434.09 Y89 4.20 7.59 Cs133 0.04 0.17 Ba138 10363.10 10318.30 La139 12.12 16.90 Ce140 12.17 15.98 Pr141 0.54 1.31 Nd146 1.35 4.66 Sm147 0.17 0.78 Eu151 7.37 7.49 Gd157 4.93 5.88 Tb159 0.01 0.10 Pb208 29.46 29.86

319 Unit CF/TSC CF/TSC CF/TSC CF/TSC CF/TSC CF/TSC CF/TSC CF/TSC CF/TSC Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral sssssssss c/i/r crrrcciii Line Numbers 789 790 791 792 793 794 795 796 797 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 5.25 5.26 5.28 5.27 5.39 5.31 5.61 5.21 5.14 Al2O3 Oxide Percents 19.91 19.81 19.77 19.81 19.78 19.99 19.84 19.50 19.83 SiO2 Oxide Percents 64.33 64.91 64.64 64.47 64.46 64.26 64.57 64.94 65.16 K2O Oxide Percents 8.62 8.10 8.38 8.64 8.42 8.07 7.63 8.61 8.60 FeO Oxide Percents 0.18 0.18 0.19 0.20 0.20 0.15 0.21 0.16 0.19 BaO Oxide Percents 1.22 1.08 1.06 1.07 1.10 1.12 0.87 0.83 1.11 CaO Oxide Percents 0.65 0.65 0.71 0.69 0.74 0.79 0.81 0.55 0.61 Oxide Totals 100.15 99.98 100.03 100.16 100.09 99.70 99.54 99.79 100.65

Na Formula Atoms 0.46 0.46 0.47 0.47 0.48 0.47 0.49 0.46 0.45 Al Formula Atoms 1.07 1.06 1.06 1.06 1.06 1.07 1.06 1.04 1.06 Si Formula Atoms 2.93 2.94 2.94 2.93 2.93 2.93 2.94 2.95 2.94 K Formula Atoms 0.50 0.47 0.49 0.50 0.49 0.47 0.44 0.50 0.50 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.01 0.02 Ca Formula Atoms 0.03 0.03 0.03 0.03 0.04 0.04 0.04 0.03 0.03 Formula Totals 13.02 12.99 13.01 13.02 13.02 13.00 13.00 13.00 13.00 100*Ca/(Ca+Na) 6.28 6.36 6.89 6.73 7.02 7.60 7.41 5.53 6.15

An 3.12 3.26 3.49 3.36 3.59 3.95 4.05 2.73 3.03 Ab 46.53 48.07 47.22 46.52 47.56 48.03 50.64 46.59 46.17 Or 50.35 48.67 49.28 50.12 48.85 48.02 45.31 50.68 50.80

Grain Average

LA-ICP-MS (ppm) Si29 Mg25 Ca43 Ti47 Rb85 Sr88 Y89 Cs133 Ba138 La139 Ce140 Pr141 Nd146 Sm147 Eu151 Gd157 Tb159 Pb208

320 Unit CF/TSC CF/TSC CF/TSC CF/TSC CAN-silver CAN-silver CAN-silver Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral ss s s s s s c/i/r ii r r r r c Line Numbers 798 799 800 801 803 804 805 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 5.25 5.33 5.07 5.21 5.28 5.40 5.10 Al2O3 Oxide Percents 19.90 19.89 20.04 19.76 19.65 19.73 19.71 SiO2 Oxide Percents 64.43 64.38 64.29 64.46 63.55 63.74 63.71 K2O Oxide Percents 8.21 8.23 8.22 8.28 8.45 8.07 8.39 FeO Oxide Percents 0.22 0.17 0.20 0.20 0.20 0.23 0.18 BaO Oxide Percents 1.22 0.98 1.24 1.09 1.06 1.08 1.04 CaO Oxide Percents 0.80 0.75 0.79 0.70 0.76 0.80 0.77 Oxide Totals 100.02 99.73 99.84 99.69 98.95 99.05 98.89

Na Formula Atoms 0.46 0.47 0.45 0.46 0.47 0.48 0.45 Al Formula Atoms 1.07 1.07 1.08 1.06 1.07 1.07 1.07 Si Formula Atoms 2.93 2.93 2.93 2.94 2.93 2.93 2.93 K Formula Atoms 0.48 0.48 0.48 0.48 0.50 0.47 0.49 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.02 0.02 0.02 0.02 0.02 0.02 0.02 Ca Formula Atoms 0.04 0.04 0.04 0.03 0.04 0.04 0.04 Formula Totals 13.01 13.01 13.00 13.00 13.02 13.02 13.01 100*Ca/(Ca+Na) 7.76 7.23 7.88 6.94 7.38 7.59 7.73

An 3.98 3.72 3.98 3.52 3.74 3.98 3.87 Ab 47.30 47.73 46.48 47.16 46.90 48.40 46.15 Or 48.72 48.55 49.55 49.32 49.36 47.62 49.98

Grain Average 3.60 47.44 48.96

LA-ICP-MS (ppm) rc r Si29 37866667.95 40079414.51 42751902.97 Mg25 14.07 7.20 22.46 Ca43 0.72 0.72 0.85 Ti47 223.58 173.01 229.80 Rb85 138.33 81.72 89.52 Sr88 206.80 208.11 229.79 Y89 0.58 0.64 0.62 Cs133 0.27 0.05 0.06 Ba138 6288.44 6767.09 6547.83 La139 8.42 8.78 11.24 Ce140 7.59 7.52 10.17 Pr141 0.37 0.37 0.55 Nd146 0.83 0.88 1.14 Sm147 0.10 0.07 0.08 Eu151 4.09 4.19 4.83 Gd157 0.16 0.16 0.22 Tb159 0.00 0.00 0.01 Pb208 37.16 35.56 36.53

321 Unit CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral s ssssss c/i/r c cccci i Line Numbers 806 824 825 826 827 828 829 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 5.38 5.50 5.36 5.25 5.34 5.28 5.36 Al2O3 Oxide Percents 19.76 19.61 19.53 19.82 19.88 19.92 19.98 SiO2 Oxide Percents 63.90 64.57 64.23 64.61 64.61 64.62 64.52 K2O Oxide Percents 7.95 8.06 8.44 8.62 8.28 8.34 8.25 FeO Oxide Percents 0.22 0.21 0.19 0.17 0.19 0.13 0.17 BaO Oxide Percents 1.12 0.87 1.00 1.00 1.25 1.11 1.15 CaO Oxide Percents 0.81 0.68 0.69 0.66 0.76 0.74 0.70 Oxide Totals 99.14 99.50 99.44 100.14 100.32 100.14 100.14

Na Formula Atoms 0.48 0.49 0.48 0.46 0.47 0.46 0.47 Al Formula Atoms 1.07 1.05 1.05 1.06 1.06 1.07 1.07 Si Formula Atoms 2.93 2.94 2.94 2.94 2.93 2.93 2.93 K Formula Atoms 0.47 0.47 0.49 0.50 0.48 0.48 0.48 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.02 0.02 0.02 0.02 0.02 0.02 0.02 Ca Formula Atoms 0.04 0.03 0.03 0.03 0.04 0.04 0.03 Formula Totals 13.01 13.01 13.02 13.02 13.01 13.01 13.01 100*Ca/(Ca+Na) 7.68 6.42 6.63 6.49 7.26 7.22 6.74

An 4.04 3.37 3.37 3.23 3.73 3.67 3.47 Ab 48.63 49.18 47.45 46.53 47.66 47.23 47.97 Or 47.33 47.45 49.18 50.24 48.61 49.10 48.56

Grain Average 3.91 47.52 48.57

LA-ICP-MS (ppm) c Si29 38537764.13 Mg25 8.49 Ca43 0.75 Ti47 230.65 Rb85 83.85 Sr88 218.76 Y89 0.63 Cs133 0.05 Ba138 6730.40 La139 9.88 Ce140 8.59 Pr141 0.43 Nd146 0.87 Sm147 0.09 Eu151 4.51 Gd157 0.10 Tb159 0.01 Pb208 34.26

322 Unit CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver CAN-silver Sample 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B 08CP21B mineral sssssss c/i/r iiiiiii Line Numbers 830 831 832 833 834 835 836 Date 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009 7/13/2009

Na2O Oxide Percents 5.22 4.83 5.04 5.21 5.17 5.43 5.23 Al2O3 Oxide Percents 19.71 19.56 19.68 19.76 19.69 19.87 19.73 SiO2 Oxide Percents 64.38 64.79 64.63 64.57 64.69 64.42 65.06 K2O Oxide Percents 8.48 9.26 8.98 8.61 8.16 8.25 8.32 FeO Oxide Percents 0.18 0.22 0.21 0.19 0.20 0.21 0.21 BaO Oxide Percents 0.97 0.91 1.12 1.16 1.05 0.85 0.91 CaO Oxide Percents 0.64 0.49 0.56 0.62 0.69 0.73 0.60 Oxide Totals 99.59 100.06 100.23 100.11 99.66 99.77 100.06

Na Formula Atoms 0.46 0.43 0.44 0.46 0.46 0.48 0.46 Al Formula Atoms 1.06 1.05 1.06 1.06 1.06 1.07 1.05 Si Formula Atoms 2.94 2.95 2.94 2.94 2.95 2.93 2.95 K Formula Atoms 0.49 0.54 0.52 0.50 0.47 0.48 0.48 Fe Formula Atoms 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Ba Formula Atoms 0.02 0.02 0.02 0.02 0.02 0.02 0.02 Ca Formula Atoms 0.03 0.02 0.03 0.03 0.03 0.04 0.03 Formula Totals 13.01 13.01 13.02 13.01 12.99 13.01 13.00 100*Ca/(Ca+Na) 6.36 5.31 5.81 6.14 6.86 6.93 5.98

An 3.18 2.42 2.76 3.04 3.49 3.59 3.02 Ab 46.78 43.14 44.76 46.44 47.37 48.25 47.41 Or 50.04 54.45 52.48 50.52 49.14 48.16 49.58

Grain Average

LA-ICP-MS (ppm) rim Si29 37528193.51 Mg25 19.42 Ca43 0.86 Ti47 244.30 Rb85 89.15 Sr88 226.40 Y89 1.13 Cs133 0.10 Ba138 7336.12 La139 10.74 Ce140 10.13 Pr141 0.44 Nd146 0.99 Sm147 0.12 Eu151 4.69 Gd157 0.82 Tb159 0.00 Pb208 36.54

323

APPENDIX L

RESOURCES FOR CHAPTER 3 – MICROPROBE ANALYSES OF PYROXENE FROM THE EUBM

Unit Canyon Canyon Canyon Canyon Canyon Canyon Canyon Canyon Sample 0934 0934 0934 0934 0934 0934 0934 0934 mineral opx 1 opx 1 opx 1 opx 1 opx 1 cpx 2 cpx 2 cpx 2 c/i/r r c c c r r c c Line Numbers 86 87 88 89 90 96 97 98 Date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 CaO 1.51 1.60 1.56 1.61 1.58 18.28 18.53 18.58 K2O Oxide Percents 0.05 0.00 0.00 0.01 0.00 0.01 0.00 0.00 SiO2 Oxide Percents 50.28 50.49 50.14 49.86 50.43 51.19 51.28 51.21 Al2O3 Oxide Percents 0.43 0.40 0.36 0.37 0.38 0.74 0.79 0.94 FeO Oxide Percents 31.02 31.21 31.85 32.19 31.23 16.62 16.18 15.91 Na2O Oxide Percents 0.06 0.04 0.05 0.05 0.01 0.31 0.32 0.30 TiO2 Oxide Percents 0.16 0.22 0.15 0.16 0.16 0.26 0.24 0.24 MgO Oxide Percents 14.31 14.40 13.96 13.58 14.39 10.82 11.23 11.47 MnO Oxide Percents 1.80 1.82 1.81 1.84 1.64 0.99 0.95 0.95 Oxide Totals 99.64 100.20 99.87 99.69 99.83 99.22 99.54 99.61

Ca 0.06 0.07 0.07 0.07 0.07 0.76 0.77 0.77 K 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Si 1.98 1.98 1.98 1.98 1.98 1.98 1.98 1.97 Al 0.02 0.02 0.02 0.02 0.02 0.03 0.04 0.04 Fe 1.02 1.02 1.05 1.07 1.03 0.54 0.52 0.51 Na 0.00 0.00 0.00 0.00 0.00 0.02 0.02 0.02 Ti 0.00 0.01 0.00 0.00 0.00 0.01 0.01 0.01 Mg 0.84 0.84 0.82 0.80 0.84 0.62 0.65 0.66 Mn 0.06 0.06 0.06 0.06 0.05 0.03 0.03 0.03 total 10.01 10.00 10.01 10.01 10.00 10.00 10.01 10.01

Wo 3.31 3.48 3.41 3.53 3.44 39.48 39.61 39.58 En 43.63 43.56 42.35 41.39 43.54 32.50 33.39 33.98 Fs 53.06 52.96 54.24 55.07 53.02 28.02 26.99 26.44

LA-ICP-MS (ppm) Si29 8851704.76 8909568.57 Ca43 1.10 1.12 Sc45 90.00 89.06 Ti47 968.67 1026.68 Rb85 0.00 0.00 Sr88 0.00 0.00 Y89 69.08 70.02 Zr90 4.70 5.17 Nb93 0.10 0.10 Cs133 0.00 0.00 Ba138 0.00 0.00 La139 0.27 0.40 Ce140 1.83 2.11 Pr141 0.50 0.49 Nd146 3.40 3.83 Sm147 2.48 2.52 Eu151 0.16 0.20 Gd157 3.90 3.85 Tb159 1.31 1.28 Dy163 10.71 10.58 Ho165 2.97 2.87 Er166 9.67 9.39 Tm169 1.66 1.68 Yb172 12.56 12.44 Lu175 2.23 2.21 Hf178 0.22 0.25 Ta181 0.00 0.00 Pb208 0.00 0.06 Th232 0.00 0.01 U238 0.00 0.01

325 Unit Canyon Canyon Canyon Canyon Canyon Canyon Canyon Canyon Sample 0934 0934 0934 0934 0934 0934 0934 0934 mineral cpx 2 cpx 3 cpx 3 cpx 3 cpx 3 cpx 3 cpx 3 cpx 3 c/i/r rrccccrr Line Numbers 99 100 101 102 103 104 105 106 Date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 CaO 18.46 18.55 18.52 18.43 18.48 18.50 18.26 18.17 K2O Oxide Percents 0.02 0.02 0.01 0.01 0.01 0.00 0.00 0.01 SiO2 Oxide Percents 51.07 51.13 50.91 51.27 51.34 51.27 50.57 50.70 Al2O3 Oxide Percents 0.97 0.68 1.02 0.97 0.92 0.75 0.67 0.70 FeO Oxide Percents 15.88 16.81 15.03 16.23 15.76 16.44 17.33 17.24 Na2O Oxide Percents 0.23 0.30 0.33 0.32 0.27 0.22 0.30 0.35 TiO2 Oxide Percents 0.29 0.22 0.30 0.33 0.32 0.23 0.18 0.20 MgO Oxide Percents 11.57 10.70 11.78 10.99 11.57 11.02 10.44 10.51 MnO Oxide Percents 0.96 1.03 0.98 1.01 0.98 0.97 1.01 1.08 Oxide Totals 99.45 99.44 98.88 99.57 99.66 99.40 98.77 98.97

Ca 0.76 0.77 0.77 0.76 0.76 0.77 0.77 0.76 K 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Si 1.97 1.98 1.97 1.98 1.97 1.98 1.98 1.98 Al 0.04 0.03 0.05 0.04 0.04 0.03 0.03 0.03 Fe 0.51 0.54 0.49 0.52 0.51 0.53 0.57 0.56 Na 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.03 Ti 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Mg 0.66 0.62 0.68 0.63 0.66 0.63 0.61 0.61 Mn 0.03 0.03 0.03 0.03 0.03 0.03 0.03 0.04 total 10.01 10.01 10.01 10.00 10.01 10.00 10.01 10.01

Wo 39.31 39.85 39.71 39.73 39.43 39.65 39.43 39.28 En 34.29 31.97 35.14 32.96 34.32 32.86 31.36 31.62 Fs 26.40 28.18 25.16 27.31 26.25 27.50 29.21 29.09

LA-ICP-MS (ppm) Si29 8054319.26 8352551.62 Ca43 15.19 15.36 Sc45 259.40 244.57 Ti47 1433.21 1276.36 Rb85 0.00 0.00 Sr88 14.01 12.75 Y89 285.68 286.58 Zr90 58.75 49.69 Nb93 0.20 0.17 Cs133 0.00 0.00 Ba138 0.31 0.24 La139 34.24 34.46 Ce140 138.27 145.67 Pr141 25.39 27.05 Nd146 141.20 148.38 Sm147 47.96 50.51 Eu151 4.30 3.98 Gd157 46.76 49.38 Tb159 9.66 9.85 Dy163 59.45 61.56 Ho165 11.91 12.47 Er166 31.53 32.48 Tm169 4.30 4.35 Yb172 26.14 25.99 Lu175 4.06 4.03 Hf178 2.50 2.28 Ta181 0.02 0.00 Pb208 0.71 0.80 Th232 0.12 0.07 U238 0.03 0.02

326 Unit Canyon Canyon Canyon Canyon Canyon Canyon Canyon Canyon Sample 0934 0934 0934 0934 0934 0934 0934 0934 mineral cpx 3 cpx 3 cpx 4 cpx 4 cpx 4 cpx 4 cpx 5 cpx 5 c/i/r rrrcrrrc Line Numbers 107 108 132 133 135 136 180 181 Date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 CaO 18.62 18.58 18.09 18.99 18.94 18.88 18.55 18.34 K2O Oxide Percents 0.01 0.00 0.07 0.00 0.01 0.01 0.00 0.02 SiO2 Oxide Percents 51.11 51.09 51.08 51.46 51.28 51.51 50.63 50.94 Al2O3 Oxide Percents 0.71 0.72 0.76 0.71 0.70 0.74 0.87 0.88 FeO Oxide Percents 16.01 16.31 17.03 16.00 16.18 15.83 15.94 16.12 Na2O Oxide Percents 0.31 0.31 0.38 0.25 0.27 0.36 0.33 0.35 TiO2 Oxide Percents 0.19 0.22 0.24 0.29 0.25 0.25 0.28 0.20 MgO Oxide Percents 10.99 10.98 10.42 11.44 11.22 11.36 11.25 11.08 MnO Oxide Percents 1.00 1.05 1.16 0.99 1.00 0.96 1.01 0.94 Oxide Totals 98.95 99.26 99.24 100.15 99.84 99.90 98.86 98.88

Ca 0.77 0.77 0.75 0.78 0.78 0.78 0.77 0.76 K 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 Si 1.98 1.98 1.98 1.97 1.97 1.98 1.97 1.98 Al 0.03 0.03 0.03 0.03 0.03 0.03 0.04 0.04 Fe 0.52 0.53 0.55 0.51 0.52 0.51 0.52 0.52 Na 0.02 0.02 0.03 0.02 0.02 0.03 0.02 0.03 Ti 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Mg 0.64 0.63 0.60 0.65 0.64 0.65 0.65 0.64 Mn 0.03 0.03 0.04 0.03 0.03 0.03 0.03 0.03 total 10.01 10.01 10.01 10.01 10.01 10.01 10.02 10.01

Wo 40.13 39.89 39.43 40.07 40.15 40.13 39.78 39.59 En 32.93 32.79 31.59 33.57 33.08 33.60 33.54 33.25 Fs 26.94 27.32 28.98 26.36 26.77 26.27 26.67 27.15

LA-ICP-MS (ppm) Si29 8006460.17 6658626.70 Ca43 15.52 16.47 Sc45 243.63 245.32 Ti47 1256.03 1178.06 Rb85 0.12 0.00 Sr88 11.75 9.19 Y89 309.05 306.58 Zr90 50.76 44.31 Nb93 0.21 0.20 Cs133 0.00 0.00 Ba138 1.19 0.56 La139 39.75 44.63 Ce140 164.26 179.52 Pr141 30.05 32.07 Nd146 164.81 173.11 Sm147 53.78 55.93 Eu151 3.99 3.56 Gd157 51.75 55.83 Tb159 10.59 11.05 Dy163 65.40 66.84 Ho165 13.18 13.41 Er166 34.24 35.01 Tm169 4.58 4.58 Yb172 26.93 26.77 Lu175 4.22 4.38 Hf178 2.43 2.16 Ta181 0.02 0.01 Pb208 1.05 0.91 Th232 0.29 0.63 U238 0.08 0.07

327 Unit Canyon Canyon Canyon Canyon Canyon Canyon Sample 0934 0934 0934 0934 0934 0934 mineral cpx 5 cpx 5 cpx 5 cpx 5 cpx 5 cpx 5 c/i/r rcrrcr Line Numbers 182 183 184 185 186 187 Date 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 11/9/2009 CaO 18.69 18.97 18.24 1.93 1.68 1.58 K2O Oxide Percents 0.02 0.00 0.01 0.01 0.00 0.02 SiO2 Oxide Percents 51.33 51.19 51.07 50.28 50.00 50.40 Al2O3 Oxide Percents 0.85 0.78 0.84 0.30 0.30 0.35 FeO Oxide Percents 16.05 16.18 16.34 31.68 31.29 31.84 Na2O Oxide Percents 0.33 0.34 0.26 0.04 0.04 TiO2 Oxide Percents 0.21 0.18 0.26 0.14 0.11 0.19 MgO Oxide Percents 11.50 11.26 11.32 14.27 14.11 14.42 MnO Oxide Percents 1.00 0.92 1.01 1.81 1.80 1.81 Oxide Totals 99.99 99.83 99.34 100.45 99.30 100.65

Ca 0.77 0.78 0.76 0.08 0.07 0.07 K 0.00 0.00 0.00 0.00 0.00 0.00 Si 1.97 1.97 1.97 1.98 1.98 1.98 Al 0.04 0.04 0.04 0.01 0.01 0.02 Fe 0.52 0.52 0.53 1.04 1.04 1.04 Na 0.02 0.03 0.02 0.00 0.00 0.00 Ti 0.01 0.01 0.01 0.00 0.00 0.01 Mg 0.66 0.65 0.65 0.84 0.83 0.84 Mn 0.03 0.03 0.03 0.06 0.06 0.06 total 10.02 10.02 10.01 10.01 10.01 10.01

Wo 39.59 40.15 39.02 4.16 3.67 3.40 En 33.88 33.14 33.68 42.69 42.93 43.15 Fs 26.53 26.72 27.30 53.16 53.40 53.45

LA-ICP-MS (ppm) Si29 8826322.37 8431987.60 Ca43 16.49 16.36 Sc45 280.75 257.41 Ti47 1264.14 1406.53 Rb85 0.00 0.02 Sr88 11.62 13.10 Y89 359.21 337.40 Zr90 49.08 59.89 Nb93 0.17 0.28 Cs133 0.00 0.00 Ba138 0.71 2.27 La139 42.46 45.61 Ce140 163.04 168.49 Pr141 32.68 31.84 Nd146 186.20 177.31 Sm147 62.94 58.29 Eu151 4.10 4.41 Gd157 63.08 56.91 Tb159 12.79 11.73 Dy163 77.93 74.23 Ho165 15.59 14.99 Er166 40.17 39.70 Tm169 5.26 5.34 Yb172 31.88 31.68 Lu175 5.26 5.00 Hf178 2.46 2.92 Ta181 0.00 0.01 Pb208 0.75 0.56 Th232 0.09 0.20 U238 0.02 0.04

328

APPENDIX M

RESOURCES FOR CHAPTER 3 – MAJOR ELEMENT DATA FROM THE EUBM

Member Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin Upper Basin

Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Tuff of Tuff of Tuff of Tuff of Sulphur Unit Creek Creek Creek Creek Creek Creek Creek Creek Creek Sulphur Creek Sulphur Creek Sulphur Creek Sulphur Creek Creek

lower Peter's Peter's Peter's Peter's Peter's N. of Sulphur top of N. of top of N. of top of N. of S. Side of stoney Locality Peter's Ridge Peter's Ridge Ridge Ridge Ridge Ridge Ridge Peter's Ridge Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. Canyon interior northing 4952944 4952997 4953027 4953056 4953073 4953099 4953207 4953283 4956628 4956402 4956461 4956461 4952198 4956404 easting (12) 543026 542937 542962 542941 542964 542954 542834 542852 547209 546753 547171 547171 543104 547269 Lithology tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff wx. Tuff tuff Source CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 07 CJP 08 CJP 08 CJP 08 CJP 08 CJP08 Age (Ma) 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 Age error 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Sample # 07CP01 07CP03 O7CP04 07CP05 07CP06 07CP07 07CP08 07CP09 07CP11 08CP10 08CP11 08CP13 08CP18 08CP36 Date 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 17-Dec-07 19-Dec-07 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 2-Jan-09 SiO2 76.19 76.12 76.32 76.07 75.97 75.98 76.08 76.02 77.92 76.74 77.36 76.89 76.51 77.26 TiO2 0.34 0.35 0.36 0.34 0.34 0.34 0.34 0.34 0.32 0.33 0.31 0.33 0.31 0.33 Al2O3 12.44 12.49 12.53 12.52 12.63 12.55 12.63 12.57 12.26 12.62 12.47 12.97 12.29 12.77 FeO* 1.77 1.92 1.68 2.02 1.95 1.97 1.83 1.90 0.51 1.29 0.80 1.10 1.69 0.74 MnO 0.02 0.03 0.03 0.03 0.02 0.02 0.02 0.02 0.01 0.02 0.01 0.00 0.03 0.02 MgO 0.07 0.05 0.05 0.07 0.05 0.05 0.07 0.04 0.03 0.06 0.06 0.08 0.06 0.05 CaO 0.69 0.65 0.67 0.66 0.67 0.67 0.66 0.66 0.53 0.58 0.54 0.50 0.69 0.56 Na2O 3.46 3.42 3.41 3.34 3.41 3.46 3.32 3.40 3.31 3.30 3.31 3.18 3.42 3.23 K2O 4.98 4.93 4.93 4.93 4.93 4.91 5.01 5.02 5.08 5.02 5.12 4.90 4.98 5.03 P2O5 0.04 0.03 0.03 0.03 0.04 0.04 0.03 0.03 0.03 0.04 0.03 0.04 0.03 0.03 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 96.54 96.59 96.48 96.28 96.29 96.53 96.66 96.46 96.74 99.21 99.14 98.71 99.68 97.54 T.A. 8.44 8.35 8.33 8.27 8.34 8.37 8.33 8.41 8.39 8.32 8.43 8.08 8.39 8.26

XRF (ppm) Ni 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.24 0.00 0.14 0.00 Cr 2.60 2.90 3.20 4.20 2.50 3.00 3.60 1.50 3.50 3.20 6.40 2.20 2.80 3.20 Sc 5.10 5.30 5.50 5.20 5.50 6.30 5.80 5.40 4.20 4.10 4.10 5.20 4.90 5.70 V 3.30 4.70 1.40 3.40 2.50 2.40 5.20 3.30 0.10 4.10 2.40 2.90 3.70 3.40 Ba 996.60 1023.50 1021.10 989.00 1042.60 987.90 999.70 1003.00 950.10 979.00 921.40 1017.60 962.60 970.30 Rb 170.90 167.30 170.00 167.10 168.50 165.20 175.60 171.50 174.40 174.70 179.90 167.70 175.50 171.50 Sr 72.10 74.30 77.70 71.90 92.90 76.50 73.90 74.90 63.70 68.00 61.10 73.80 66.90 65.50 Zr 362.10 370.90 375.70 362.30 370.00 368.50 369.50 364.90 356.80 365.60 352.50 367.60 349.70 367.60 Y 44.60 58.00 54.60 47.20 50.70 57.80 42.20 51.30 62.00 57.60 59.40 74.80 62.00 61.40 Nb 47.60 47.50 47.90 47.30 48.00 47.80 47.40 48.40 49.30 50.30 50.80 48.80 49.30 50.10 Ga 20.10 20.70 20.00 20.70 20.80 19.90 19.30 20.70 19.10 20.40 20.60 20.90 19.90 19.90 Cu 0.70 0.20 0.40 -0.90 -1.40 0.40 0.90 0.60 0.20 0.00 0.00 0.00 0.50 0.00 Zn 73.60 67.50 71.10 65.00 34.60 69.50 67.30 65.70 22.50 45.60 30.70 55.60 56.50 35.70 Pb 39.00 35.20 58.40 32.30 32.70 31.30 28.30 28.90 29.30 35.10 23.40 31.70 25.20 32.00 La 57.50 73.60 75.30 58.00 70.80 67.40 61.10 60.80 73.60 84.90 74.00 87.80 75.70 78.50 Ce 104.70 136.80 149.20 136.10 110.40 138.60 108.50 137.80 147.00 171.40 140.30 166.50 136.00 166.40 Th 23.40 23.40 23.90 22.90 24.30 23.50 23.70 23.30 26.40 26.50 26.50 25.60 24.80 27.10 Nd 46.10 63.70 61.70 52.80 50.70 58.60 49.40 48.70 61.50 73.90 60.30 66.80 58.70 64.60 U 5.10 5.60 6.20 5.00 5.00 5.90 5.50 5.40 6.70 5.80 6.50 6.60 6.00 5.20

ICP-MS (ppm) La 63.84 77.75 78.90 63.13 78.94 72.37 63.45 64.48 79.12 89.21 75.84 89.58 76.60 81.48 Ce 110.90 139.07 153.89 139.47 118.05 139.91 111.02 140.70 152.34 167.67 144.87 164.09 137.39 165.13 Pr 13.50 17.58 17.40 14.56 15.19 16.53 13.81 13.84 17.93 20.45 17.19 18.56 16.81 18.71 Nd 48.52 64.30 63.40 53.32 54.62 60.52 50.42 49.88 67.27 74.79 62.24 67.32 60.77 67.53 Sm 9.92 13.48 13.23 11.20 11.04 12.65 10.35 10.34 13.91 14.81 12.96 13.74 12.61 13.97 Eu 1.90 1.98 2.00 1.98 1.96 1.99 2.00 1.92 1.93 1.93 1.72 2.11 1.75 1.88 Gd 8.76 12.16 11.89 10.01 9.85 11.45 9.01 9.22 12.82 12.57 11.44 12.85 11.27 12.26 Tb 1.54 2.09 2.02 1.71 1.66 1.95 1.54 1.59 2.13 2.02 1.93 2.20 1.92 2.12 Cy 9.39 12.54 11.91 10.23 10.16 11.82 9.24 9.82 12.73 11.95 11.85 13.75 11.75 12.64 Ho 1.88 2.41 2.32 2.00 1.98 2.31 1.80 2.01 2.51 2.29 2.36 2.76 2.36 2.49 Er 5.27 6.44 6.16 5.40 5.50 6.25 4.87 5.53 6.68 6.13 6.42 7.60 6.41 6.78 Tm 0.77 0.92 0.87 0.78 0.80 0.91 0.71 0.82 0.96 0.87 0.93 1.10 0.93 0.98 Yb 4.76 5.49 5.32 4.75 4.94 5.56 4.34 4.99 5.85 5.46 5.70 6.73 5.75 6.01 Lu 0.75 0.81 0.80 0.71 0.77 0.84 0.66 0.76 0.87 0.81 0.87 1.04 0.88 0.93 Ba 1039.26 1064.63 1053.00 1020.35 1077.06 1020.40 1018.02 1031.51 975.18 983.25 926.21 1031.60 971.70 997.58 Th 24.29 23.91 23.82 23.55 24.09 23.46 23.32 23.72 25.35 23.86 25.04 23.61 24.21 25.18 Nb 49.34 49.00 49.16 48.58 48.46 48.72 48.07 49.25 51.11 49.63 49.90 48.29 48.63 50.81 Y 45.09 58.38 54.41 46.30 49.89 56.99 41.72 51.31 61.20 56.57 58.16 73.70 60.08 61.30 Hf 10.91 10.96 10.99 10.67 10.82 10.63 10.80 10.79 10.75 10.75 10.49 10.85 10.32 11.03 Ta 3.46 3.42 3.41 3.39 3.38 3.40 3.33 3.44 3.56 3.50 3.56 3.43 3.49 3.54 U 6.04 5.83 5.88 5.60 5.86 5.88 5.49 5.91 6.44 5.90 6.22 6.11 5.79 6.23 Pb 35.52 34.21 56.89 31.43 32.38 30.30 27.34 27.72 28.16 35.04 23.70 30.77 25.84 31.66 Rb 175.93 169.51 171.05 169.16 169.81 167.79 176.38 174.56 178.69 176.65 180.45 169.03 176.52 174.95 Cs 2.83 3.25 2.94 2.86 2.56 3.35 3.49 3.77 3.74 3.35 3.27 2.76 3.29 3.57 Sr 74.46 75.46 77.83 71.57 92.70 76.74 73.97 76.02 63.53 67.86 60.87 73.85 68.01 66.67 Sc 5.13 5.30 5.45 5.65 5.37 6.18 5.67 6.16 4.36 6.25 5.04 5.79 4.59 5.63 Zr 363.47 368.03 374.08 362.54 368.91 358.26 366.70 366.67 358.92 371.38 354.06 370.08 346.08 377.84

330 Upper Upper Upper Upper Upper Member Upper Basin Upper Basin Upper Basin Basin Upper Basin Basin Basin Basin Basin Upper Basin Upper Basin Upper Basin Upper Basin

Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Sulphur Sulphur Sulphur Sulphur Upper Tuff of Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Unit Creek Creek Creek Creek Sulphur Creek Creek Creek Creek Creek Creek Creek Creek Creek

low Upper TSC - vitrophyre basal ash basal ash Top of Unit - basal ash basal ash basal ash basal ash lower stoney N. Canyon N. Canyon Wapiti Wapiti Lake N. of flow, N.of flow, N.of Wapiti Lake flow, N.of flow, N.of flow, N.of flow, N.of Locality interior rim rim Lake Trail Trail Sulphur Ck. Sulphur Ck. Sulphur Ck. Trail Sulphur Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. northing 4956428 4953445 4953445 4949629 4949775 4956569 4956400 4956400 4949636 4956392 4956392 4956392 4956392 easting (12) 547312 543881 543881 555977 556089 547207 547245 547245 555963 547242 547242 547242 547242 Lithology tuff tuff tuff tuff tuff vitrophyre vitrophyre vitrophyre vitric ignimbrite ignimbrite ignimbrite ignimbrite Source CJP08 CJP08 CJP08 CJP09 CJP09 CJP 07 CJP08 CJP08 CJP09 CJP 08 CJP 08 CJP 08 CJP 08 Age (Ma) 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 Age error 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 Sample # 08CP37 08CP39 08CP40 0939 0940 07CP12 08CP34 08CP35 0938 08CP27WR 08CP28WR 08CP29WR 08CP31WR Date 2-Jan-09 2-Jan-09 2-Jan-09 6-Sep-09 6-Sep-09 19-Dec-07 1-Jan-09 2-Jan-09 9/6/2009 29-Dec-08 30-Dec-08 31-Dec-08 31-Dec-08 SiO2 77.26 76.03 75.97 76.01 76.029 76.90 76.58 76.99 75.17 77.23 77.19 83.18 76.91 TiO2 0.35 0.35 0.35 0.36 0.340 0.31 0.31 0.30 0.38 0.33 0.31 0.18 0.27 Al2O3 12.71 12.56 12.69 12.73 12.459 12.40 12.37 12.32 12.99 12.68 12.80 9.35 13.16 FeO* 0.61 1.93 1.84 1.55 1.748 1.40 1.71 1.41 2.14 1.31 1.22 0.75 1.28 MnO 0.00 0.02 0.02 0.05 0.043 0.03 0.04 0.03 0.05 0.03 0.03 0.02 0.03 MgO 0.04 0.03 0.04 0.11 0.125 0.05 0.06 0.04 0.14 0.10 0.08 0.03 0.06 CaO 0.60 0.66 0.66 0.82 0.871 0.56 0.67 0.58 0.96 0.72 0.69 0.50 0.62 Na2O 3.37 3.39 3.41 3.49 3.445 3.11 3.06 3.11 3.51 2.71 2.67 2.17 2.71 K2O 5.02 4.99 5.00 4.84 4.907 5.20 5.18 5.18 4.63 4.88 5.00 3.80 4.93 P2O5 0.04 0.03 0.03 0.04 0.033 0.04 0.02 0.02 0.03 0.02 0.02 0.01 0.02 Total 100.00 100.00 100.00 100.00 100.000 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 99.17 98.80 98.32 97.96 97.115 94.57 95.86 96.88 97.60 96.38 95.89 96.64 95.21 T.A. 8.39 8.39 8.40 8.33 8.352 8.31 8.24 8.29 8.14 7.59 7.67 5.97 7.65

XRF (ppm) Ni 1.02 0.34 0.01 1.60 2.100 0.00 1.31 0.45 2.40 0.00 0.00 0.00 0.00 Cr 4.40 3.10 3.30 4.40 4.300 2.30 4.50 4.10 5.50 8.30 5.80 3.00 4.60 Sc 5.60 5.90 5.40 8.40 6.300 3.80 5.60 5.30 6.50 5.30 4.90 3.80 5.90 V 3.50 3.60 4.00 5.10 4.700 2.50 3.70 2.40 8.00 6.60 6.20 2.60 16.60 Ba 995.60 1064.00 1081.50 1068.20 1029.100 881.60 864.10 898.30 1102.20 966.40 939.00 847.40 955.70 Rb 175.80 171.20 168.90 166.80 167.900 176.00 176.40 177.20 153.20 171.70 174.70 126.90 167.30 Sr 67.70 75.30 78.10 90.90 81.100 58.70 56.60 54.70 101.00 69.90 65.70 44.30 56.30 Zr 388.40 375.40 379.10 400.60 384.000 329.00 340.00 335.60 406.80 348.60 329.90 195.80 287.80 Y 71.00 62.50 46.60 55.50 58.000 64.30 67.30 63.80 76.80 61.00 59.50 43.60 52.90 Nb 50.90 49.00 48.50 47.90 48.300 48.80 49.10 48.70 46.90 46.50 45.80 31.40 41.90 Ga 21.50 20.50 21.20 19.90 19.700 20.30 18.80 18.90 20.50 19.70 20.50 15.10 19.30 Cu 0.90 0.50 0.80 2.00 1.700 0.30 0.70 0.00 1.90 0.00 0.00 0.00 0.00 Zn 26.20 56.80 70.20 57.20 55.100 54.30 66.70 58.50 71.60 58.50 61.00 43.60 69.90 Pb 31.00 30.40 29.30 31.30 29.500 31.70 31.20 31.10 29.60 30.60 28.40 20.70 27.40 La 94.40 75.90 71.20 76.10 74.400 88.70 80.80 80.70 77.30 70.50 69.80 51.70 64.50 Ce 193.40 146.80 135.60 146.70 142.800 179.80 157.20 158.00 145.80 138.60 133.80 98.40 119.80 Th 26.90 25.30 23.80 23.90 24.200 25.30 24.60 25.40 22.70 23.70 23.80 17.30 21.70 Nd 77.40 63.80 56.70 57.40 58.200 66.50 64.30 62.40 64.90 55.10 52.60 38.00 46.50 U 5.60 4.60 4.20 5.30 5.900 6.60 6.90 4.40 7.00 5.30 5.00 3.30 5.90

ICP-MS (ppm) La 94.80 77.20 74.40 78.09 76.516 95.04 81.25 83.18 80.74 74.13 71.89 51.07 62.02 Ce 193.80 150.39 137.55 152.19 145.763 189.43 159.94 161.83 155.12 140.96 136.69 97.82 119.25 Pr 22.19 18.02 16.36 17.07 16.336 20.96 18.49 18.44 18.37 15.77 15.30 11.08 13.21 Nd 81.32 66.12 58.91 61.82 59.148 71.73 67.40 65.41 68.58 56.08 54.75 40.00 47.61 Sm 16.80 13.90 12.06 12.52 12.074 14.08 13.97 13.21 14.70 11.38 11.21 8.26 9.77 Eu 1.98 1.95 1.98 2.10 1.940 1.55 1.67 1.54 2.39 1.62 1.59 1.13 1.35 Gd 15.15 12.48 10.38 11.33 10.844 12.48 12.46 11.88 14.18 10.59 10.22 7.60 9.30 Tb 2.57 2.12 1.76 1.92 1.870 2.09 2.15 2.05 2.46 1.83 1.78 1.30 1.59 Cy 14.83 12.68 10.42 11.59 11.405 12.66 12.98 12.40 14.94 11.36 11.10 8.15 9.84 Ho 2.89 2.49 1.99 2.29 2.279 2.52 2.57 2.50 3.01 2.32 2.26 1.64 2.02 Er 7.37 6.67 5.28 6.19 6.207 6.96 7.02 6.75 8.04 6.45 6.33 4.63 5.61 Tm 1.06 0.97 0.75 0.90 0.911 1.01 1.04 0.99 1.17 0.94 0.93 0.66 0.83 Yb 6.35 5.90 4.63 5.54 5.651 6.17 6.41 6.09 7.17 5.93 5.82 4.15 5.14 Lu 0.93 0.90 0.70 0.84 0.863 0.95 0.99 0.94 1.10 0.90 0.89 0.63 0.79 Ba 1020.28 1083.61 1107.86 1101.05 1055.591 914.73 888.80 910.43 1138.14 983.60 958.50 861.22 987.34 Th 25.17 24.24 23.74 23.27 23.798 25.10 24.68 25.40 22.44 23.07 22.49 16.02 21.75 Nb 51.20 49.40 49.42 48.72 49.221 50.19 49.74 50.15 47.53 47.28 47.09 31.57 42.94 Y 69.52 62.49 46.07 53.48 56.143 64.23 67.46 63.74 74.15 60.79 60.67 43.48 52.12 Hf 11.05 11.01 11.12 11.34 10.981 10.15 10.32 10.24 11.51 10.31 9.96 6.30 9.10 Ta 3.57 3.41 3.41 3.39 3.440 3.53 3.46 3.55 3.28 3.32 3.24 2.21 3.07 U 6.64 5.80 5.14 5.88 5.884 6.25 6.09 6.16 5.85 5.50 5.36 3.88 5.04 Pb 30.30 30.75 28.74 38.68 29.284 31.98 31.29 31.94 30.49 30.36 28.48 21.06 28.50 Rb 178.06 173.92 172.57 166.18 167.427 178.97 178.96 180.68 153.53 177.10 186.32 135.32 169.49 Cs 2.66 2.73 3.00 3.57 3.181 4.87 4.97 4.79 3.63 9.26 7.39 6.55 6.69 Sr 67.77 76.15 78.89 90.37 79.841 59.18 57.87 55.91 99.68 71.48 68.39 46.65 56.98 Sc 5.83 5.95 6.18 8.51 6.846 5.48 5.72 5.33 7.07 5.76 6.33 3.93 5.64 Zr 382.97 373.69 384.83 410.13 396.594 333.49 345.90 341.32 418.14 350.71 340.94 202.29 294.24

331 Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Member Upper Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin

Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Tuff of Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Sulphur Canyon Unit Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Creek Flow

basal ash basal ash top of N. top of N. top of N. top of N. basal ash basal ash basal ash basal ash basal ash basal ash flow, N.of flow, N.of of Sulphur of Sulphur of Sulphur of Sulphur flow, N.of flow, N.of flow, N.of flow, N.of flow, N.of flow, N.of lithic layer Peter's Locality Sulphur Ck. Sulphur Ck. Ck. Ck. Ck. Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. Sulphur Ck. in basal ash Ridge northing 4956392 4956398 4956461 4956553 4956553 4956666 4956392 4956392 4956392 4956392 4956392 4956392 4956392 4953311 easting (12) 547242 547247 547171 547154 547154 547140 547242 547242 547242 547242 547242 547242 547242 542889 Lithology ignimbrite ignimbrite breccia breccia breccia breccia pumice pumice pumice pumice pumice pumice glass tuff Source CJP 08 CJP08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP 07 Age (Ma) 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.479 0.484 Age error 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.015 Sample # 08CP32WR 08CP33 08CP12 08CP14 08CP15 08CP16 08CP27P 08CP28P 08CP29P 08CP30P 08CP31P 08CP32P 08CP30G 07CP10 Date 1-Jan-09 1-Jan-09 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 29-Dec-08 30-Dec-08 31-Dec-08 31-Dec-08 1-Jan-09 1-Jan-09 31-Dec-08 12/19/2007 SiO2 76.95 76.50 76.24 77.29 75.59 75.89 89.25 88.65 82.56 84.29 89.56 77.44 77.65 75.98 TiO2 0.33 0.34 0.38 0.32 0.41 0.36 0.16 0.19 0.24 0.17 0.11 0.33 0.12 0.35 Al2O3 12.97 13.42 13.12 12.51 13.29 12.77 6.07 6.52 9.95 9.13 6.03 12.86 11.99 12.41 FeO* 1.16 1.33 0.83 0.63 1.21 1.63 0.43 0.44 0.69 0.68 0.29 0.99 1.12 2.03 MnO 0.03 0.03 0.02 0.02 0.03 0.03 0.02 0.02 0.03 0.02 0.01 0.03 0.03 0.03 MgO 0.05 0.07 0.18 0.08 0.23 0.14 0.02 0.00 0.04 0.04 0.00 0.09 0.04 0.10 CaO 0.77 0.77 0.98 0.62 1.10 0.83 0.40 0.41 0.65 0.42 0.27 0.71 0.45 0.74 Na2O 2.73 2.71 3.55 3.42 3.54 3.47 1.16 1.08 1.90 1.50 0.96 2.35 3.28 3.45 K2O 4.98 4.79 4.67 5.07 4.57 4.82 2.49 2.68 3.93 3.72 2.75 5.18 5.31 4.87 P2O5 0.02 0.02 0.02 0.03 0.03 0.03 0.01 0.01 0.01 0.01 0.01 0.02 0.01 0.04 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 95.68 94.59 99.33 100.14 99.33 99.48 97.32 95.35 95.37 94.68 95.72 95.01 98.10 96.38 T.A. 7.71 7.51 8.22 8.49 8.11 8.30 3.65 3.76 5.83 5.22 3.71 7.53 8.59 8.32

XRF (ppm) Ni 0.00 0.00 2.12 2.87 0.00 0.97 0.00 2.97 2.28 0.87 5.29 1.46 0.12 0.00 Cr 5.00 7.90 10.30 3.90 8.50 5.20 3.50 4.60 3.70 3.90 2.60 4.90 3.80 3.50 Sc 5.50 7.00 5.50 6.70 6.70 6.10 3.60 2.60 2.80 3.60 2.40 4.90 4.20 6.30 V 5.80 10.00 7.60 3.80 6.20 4.50 3.50 1.90 5.40 5.60 0.30 3.90 0.00 3.10 Ba 910.10 883.50 1152.20 1002.00 1241.10 1073.80 741.90 783.30 1055.60 800.40 513.30 925.40 639.30 999.70 Rb 173.40 168.20 151.50 175.70 147.10 162.70 86.30 94.60 129.30 128.60 98.30 178.00 179.70 166.40 Sr 68.50 75.20 110.50 71.00 125.10 85.70 44.20 44.50 70.10 38.40 22.10 63.30 15.10 79.30 Zr 351.00 353.40 404.70 363.50 432.10 393.50 175.10 192.50 251.30 174.60 116.10 332.80 188.90 371.60 Y 59.50 55.70 54.40 50.30 52.00 60.40 31.10 34.50 47.40 45.90 30.60 60.90 51.50 53.60 Nb 47.70 46.00 46.50 50.70 45.70 49.60 23.40 25.10 35.20 30.50 21.90 47.80 33.00 48.00 Ga 20.60 19.70 21.50 20.20 22.60 20.80 10.10 9.60 15.10 14.80 9.70 20.10 19.40 19.60 Cu 0.00 0.70 1.20 0.00 1.00 0.70 0.00 0.00 0.00 0.00 0.00 0.60 0.00 1.20 Zn 66.30 74.50 31.10 17.40 36.50 59.10 40.90 34.90 45.30 52.50 35.60 57.40 52.90 77.10 Pb 27.40 19.80 25.30 30.90 26.50 30.00 13.90 13.10 18.90 17.20 13.70 24.90 30.10 33.20 La 72.50 66.20 71.50 71.60 74.20 81.00 36.10 44.80 59.70 51.30 37.80 73.30 63.40 68.80 Ce 131.80 125.00 133.90 130.10 137.60 142.40 73.30 77.30 102.40 102.20 69.80 135.00 114.40 130.90 Th 24.10 23.90 24.60 26.50 22.30 24.80 12.70 14.00 19.00 16.90 13.30 23.80 21.50 23.80 Nd 51.90 50.50 56.30 52.90 55.30 61.00 28.30 28.80 41.40 39.60 27.10 53.60 45.40 61.20 U 5.50 5.00 4.70 6.80 6.20 7.20 2.80 3.70 4.70 4.10 2.20 6.30 4.90 4.70

ICP-MS (ppm) La 69.60 68.16 72.76 70.59 71.92 80.22 37.64 41.64 57.89 52.02 35.95 72.68 63.27 74.56 Ce 133.34 128.85 136.01 132.86 134.96 147.02 71.59 80.30 110.50 101.81 69.38 139.26 121.72 133.04 Pr 15.06 14.58 16.01 15.37 15.27 17.90 8.09 9.11 12.55 11.60 7.84 15.73 13.71 16.98 Nd 54.51 52.18 57.86 54.95 55.13 65.08 29.20 33.04 45.41 42.05 27.91 56.42 48.97 62.47 Sm 11.15 10.69 11.98 11.11 11.26 13.36 5.85 6.81 9.13 8.65 5.72 11.44 10.25 12.91 Eu 1.61 1.61 2.31 1.76 2.47 2.09 0.93 0.99 1.57 0.99 0.60 1.56 0.70 1.95 Gd 10.43 9.78 10.41 9.54 9.77 11.77 5.45 6.14 8.60 8.28 5.34 10.58 9.39 11.63 Tb 1.82 1.71 1.74 1.65 1.65 2.02 0.93 1.06 1.50 1.45 0.92 1.85 1.66 1.96 Cy 11.23 10.45 10.67 10.06 10.17 12.24 5.70 6.48 9.08 8.70 5.64 11.35 10.01 11.64 Ho 2.28 2.14 2.12 1.98 2.00 2.41 1.17 1.30 1.84 1.75 1.15 2.31 2.02 2.23 Er 6.40 5.87 5.68 5.44 5.49 6.44 3.22 3.55 5.03 4.84 3.12 6.41 5.40 5.96 Tm 0.95 0.87 0.84 0.82 0.81 0.94 0.47 0.52 0.74 0.72 0.47 0.95 0.80 0.87 Yb 5.85 5.40 5.15 5.16 4.97 5.78 2.93 3.19 4.58 4.43 2.85 5.84 4.88 5.21 Lu 0.91 0.84 0.79 0.78 0.77 0.86 0.45 0.49 0.71 0.68 0.44 0.91 0.74 0.79 Ba 934.22 914.10 1163.05 1003.55 1256.85 1082.38 745.12 811.57 1100.04 832.77 524.89 961.31 664.10 1032.56 Th 23.18 22.66 22.36 24.94 21.27 23.22 11.30 12.14 17.87 16.64 11.93 23.49 21.07 23.26 Nb 48.25 47.45 46.05 50.07 45.64 49.13 23.83 26.27 36.47 31.42 22.03 48.75 34.94 48.74 Y 60.56 56.28 53.10 48.51 51.42 59.99 30.69 33.71 47.56 46.42 29.65 60.85 52.26 53.00 Hf 10.49 10.57 11.60 10.84 12.08 11.32 5.37 5.76 7.74 6.08 4.01 10.30 7.07 10.80 Ta 3.36 3.30 3.24 3.56 3.14 3.43 1.66 1.78 2.58 2.30 1.58 3.42 2.56 3.36 U 5.65 5.32 5.68 6.22 5.37 5.80 2.82 2.98 4.33 4.00 2.84 5.78 4.72 5.72 Pb 28.06 21.01 25.37 30.97 26.03 30.31 13.82 14.17 19.38 17.75 13.22 25.96 31.31 32.01 Rb 176.99 171.11 152.02 174.46 150.47 164.25 91.99 102.04 134.67 134.30 101.90 184.13 184.97 169.34 Cs 8.29 8.99 3.73 3.27 3.17 3.39 4.31 6.03 5.61 6.60 5.80 8.20 3.73 3.66 Sr 71.37 77.09 110.49 70.35 126.01 86.73 45.72 46.45 71.77 40.47 23.47 64.85 16.44 79.05 Sc 5.79 6.94 6.46 5.96 7.02 6.83 3.04 3.31 3.93 4.04 2.32 5.45 4.01 6.08 Zr 357.52 359.15 404.15 364.76 439.57 394.64 185.94 206.50 263.16 185.42 121.97 343.44 195.01 367.75

332 Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Basin Upper Upper Member Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Member Basin Basin Canyon Canyon Flow - Flow - Canyon Canyon Canyon Canyon Canyon Canyon Canyon Canyon Silver Cord Silver Cord Canyon Canyon Canyon Canyon Canyon Canyon Unit Flow Flow Flow Flow Flow Flow Flow Flow flow flow Flow Flow Flow Flow Flow Flow

paleo- valley S. small ridge 7-mile hole 7-mile hole S. Side of S. Side of S. Side of S. Side of S. Side of S. Side of S. Side of side of N. Canyon N. Canyon Canyon in ring Canyon Locality trail trail Canyon Canyon Canyon Canyon Canyon Canyon Canyon canyon rim rim Village fracture Flow northing 4954799 4953276 4955312 4952305 4952454 4952592 4952592 4952592 4952622 4953147 4951810 4953835 4953094 4953342 4955210 4954397 easting (12) 543870 543069 542242 543470 543589 543742 543742 543742 543804 544638 542014 544298 542915 540482 541831 542341 Lithology tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff vitric tuff wx tuff tuff tuff altered Source CJP 07 CJP 07 CJP 08 CJP 09 CJP 08 CJP 09 CJP 09 CJP 09 CJP 09 CJP 09 CJP 08 CJP08 CJP08 CJP08 CJP09 CJP09 Age (Ma) 0.484 0.484 0.484 0.484 0.479 0.484 0.484 0.484 0.484 0.484 0.484 4.84 4.84 4.84 0.484 0.484 Age error 0.015 0.015 0.015 0.015 0.01 0.015 0.015 0.015 0.015 0.015 0.015 0.01 0.01 0.01 0.015 0.015 Sample # 07CP13 07CP14 08CP06 08CP19 08CP20 08CP21A 08CP21B 08CP21C 08CP22 08CP23 08CP26 08CP41 08CP43 08CP55 0911 0917 Date 12/19/2007 12/19/2007 12/28/2008 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 29-Dec-08 12/29/2008 12/29/2008 12/29/2008 1/2/2009 1/2/2009 1/3/2009 9/6/2009 9/6/2009 SiO2 75.84 75.93 75.79 77.12 77.04 77.11 76.92 77.25 75.99 76.29 76.55 76.28 75.92 76.18 75.75 76.63 TiO2 0.35 0.34 0.35 0.21 0.25 0.19 0.23 0.19 0.31 0.34 0.34 0.32 0.33 0.33 0.34 0.23 Al2O3 12.54 12.61 12.57 12.14 12.24 12.14 12.15 12.13 12.45 12.41 12.64 12.60 12.58 12.65 12.61 12.50 FeO* 2.19 1.96 1.95 1.52 1.53 1.42 1.76 1.35 2.08 1.77 1.35 1.69 1.99 1.61 1.93 1.40 MnO 0.03 0.04 0.08 0.03 0.02 0.04 0.03 0.03 0.06 0.02 0.03 0.03 0.03 0.02 0.05 0.03 MgO 0.04 0.08 0.11 0.04 0.04 0.06 0.07 0.06 0.14 0.05 0.07 0.04 0.06 0.04 0.08 0.06 CaO 0.66 0.66 0.76 0.43 0.45 0.51 0.48 0.48 0.72 0.68 0.83 0.72 0.72 0.75 0.83 0.60 Na2O 3.38 3.41 3.50 3.30 3.26 3.38 3.29 3.33 3.42 3.43 2.50 3.44 3.47 3.46 3.52 3.46 K2O 4.93 4.93 4.86 5.19 5.14 5.14 5.04 5.17 4.80 4.96 5.65 4.87 4.88 4.91 4.83 5.06 P2O5 0.04 0.03 0.03 0.02 0.02 0.02 0.02 0.02 0.03 0.04 0.02 0.02 0.03 0.04 0.05 0.03 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 96.09 96.74 99.42 99.72 99.70 99.73 99.36 99.81 99.44 100.23 96.17 98.68 98.55 98.49 97.79 97.55 T.A. 8.30 8.34 8.36 8.49 8.41 8.52 8.34 8.50 8.22 8.40 8.15 8.31 8.35 8.37 8.35 8.52

XRF (ppm) Ni 0.00 0.00 0.88 2.33 0.15 1.53 1.35 0.97 0.33 0.00 0.00 0.08 0.21 3.36 1.90 3.00 Cr 2.90 2.80 3.70 3.30 3.80 4.00 2.40 4.10 6.20 3.50 3.70 3.90 3.10 3.80 4.10 4.10 Sc 6.10 6.40 6.10 4.30 4.50 4.60 5.90 4.00 4.30 5.40 5.20 3.50 5.80 6.80 6.00 5.70 V 2.50 4.60 5.00 0.90 2.20 0.20 1.80 1.10 3.10 2.20 1.50 3.80 2.00 4.50 2.00 3.90 Ba 1004.70 989.10 1047.30 799.00 859.70 830.60 884.10 850.70 1021.00 1038.00 1016.00 1019.20 1020.10 1026.60 1031.40 866.30 Rb 165.90 167.10 164.70 174.40 176.80 171.00 170.80 173.60 162.50 174.00 180.90 167.60 166.20 165.60 164.10 168.80 Sr 73.40 75.40 77.20 38.30 49.30 38.40 49.80 39.90 77.70 79.00 81.70 79.20 78.10 79.00 86.00 54.70 Zr 387.70 369.00 386.90 270.60 290.90 239.30 273.20 237.20 330.40 382.20 369.40 357.90 366.80 375.70 378.10 285.80 Y 60.50 54.00 61.80 57.50 42.00 52.20 46.30 54.00 59.90 58.50 65.30 58.60 56.50 61.60 62.90 57.80 Nb 48.00 48.30 49.90 41.90 46.10 38.90 42.60 40.60 44.20 49.70 47.90 48.50 48.70 49.30 48.30 42.10 Ga 20.30 20.80 20.70 20.20 18.70 19.90 20.60 18.40 20.20 20.80 20.50 20.80 20.80 20.40 20.60 20.10 Cu -0.10 1.60 1.20 0.00 0.00 0.20 0.40 0.00 1.70 0.00 0.00 0.00 0.00 0.80 2.00 1.80 Zn 65.00 71.40 84.00 48.20 46.10 55.90 57.50 50.40 75.80 75.10 58.00 58.20 72.20 87.20 74.30 49.60 Pb 27.40 37.60 31.50 28.90 28.80 27.60 28.50 28.30 32.50 29.10 30.60 29.90 28.60 29.90 31.50 32.00 La 70.00 71.00 80.80 71.90 64.60 66.40 72.10 64.40 74.40 78.70 78.80 77.80 74.60 76.70 83.60 76.70 Ce 134.30 144.90 157.10 151.70 110.40 129.20 129.20 123.30 143.20 130.50 145.20 156.00 145.30 146.70 144.00 153.30 Th 23.60 24.60 25.50 24.80 25.00 21.70 23.20 23.30 22.80 24.90 24.70 23.70 24.80 24.80 22.70 22.50 Nd 59.10 58.40 61.50 59.80 46.20 49.60 52.00 48.90 55.50 60.40 60.10 62.50 57.10 62.90 63.20 59.70 U 5.60 5.40 6.60 7.00 6.40 4.80 5.70 5.30 6.20 5.50 6.70 6.30 7.00 6.80 6.40 5.10 1.80 1.10 ICP-MS (ppm) La 75.26 76.67 79.75 73.49 63.47 66.03 68.61 65.27 71.87 78.69 78.43 80.70 73.96 77.70 81.83 79.47 Ce 139.91 150.57 155.50 146.61 113.09 129.65 128.43 123.23 138.93 133.07 150.32 154.47 146.64 150.01 147.35 158.19 Pr 16.72 16.78 17.52 16.55 13.84 14.49 14.80 14.17 15.63 17.50 17.00 17.76 16.19 18.26 17.95 17.39 Nd 61.32 60.29 63.92 59.42 49.60 52.13 52.92 50.96 56.17 63.42 61.35 64.08 58.73 66.03 65.62 62.50 Sm 12.77 12.52 13.12 12.33 10.19 10.86 10.70 10.60 11.50 12.99 12.65 13.11 12.15 13.58 13.43 12.71 Eu 1.93 1.89 1.96 1.21 1.43 1.13 1.33 1.14 1.73 1.97 1.91 2.01 1.93 1.99 2.12 1.50 Gd 11.64 11.01 11.61 10.81 8.83 9.84 9.21 9.73 10.57 11.55 11.63 11.70 10.98 11.73 12.20 11.42 Tb 1.98 1.91 1.98 1.85 1.47 1.66 1.58 1.65 1.81 1.95 1.96 2.00 1.85 1.99 2.08 1.93 Cy 11.97 11.43 12.25 11.17 8.87 10.16 9.45 10.12 11.20 11.70 12.12 11.88 11.15 11.82 12.37 11.62 Ho 2.38 2.26 2.41 2.19 1.75 2.03 1.87 2.03 2.28 2.31 2.44 2.37 2.30 2.37 2.47 2.25 Er 6.42 6.13 6.61 5.90 4.79 5.47 4.95 5.57 6.24 6.19 6.86 6.39 6.20 6.50 6.50 6.04 Tm 0.93 0.89 0.96 0.85 0.69 0.80 0.73 0.82 0.91 0.88 0.99 0.93 0.90 0.94 0.96 0.87 Yb 5.71 5.44 5.94 5.35 4.36 4.91 4.49 5.09 5.72 5.35 6.17 5.73 5.55 5.75 5.93 5.38 Lu 0.87 0.82 0.91 0.78 0.67 0.75 0.68 0.77 0.87 0.80 0.95 0.86 0.85 0.87 0.90 0.80 Ba 1032.15 1019.33 1052.63 800.89 870.20 832.79 890.53 849.73 1015.80 1037.00 1034.40 1043.48 1033.39 1042.37 1061.89 901.52 Th 23.48 23.67 24.00 23.13 23.30 21.83 22.28 22.18 21.77 23.73 23.56 23.84 23.58 23.99 23.04 22.34 Nb 49.30 49.14 49.27 40.61 45.08 37.63 41.35 39.30 42.97 48.09 48.45 48.91 48.86 49.37 48.09 42.94 Y 60.04 53.24 60.38 54.20 39.80 49.48 44.25 51.86 58.82 55.00 63.83 58.58 55.65 59.94 60.58 55.56 Hf 10.98 10.80 11.25 8.62 8.97 7.91 8.57 7.77 9.53 10.95 10.75 10.53 10.68 10.81 10.77 9.14 Ta 3.40 3.44 3.46 3.00 3.28 2.79 3.02 2.87 3.05 3.45 3.41 3.37 3.44 3.44 3.34 3.02 U 5.62 5.81 6.20 5.50 5.39 5.15 5.31 5.26 5.51 5.86 5.85 5.98 5.91 6.55 5.76 5.41 Pb 27.22 37.39 31.31 27.98 29.16 28.93 28.10 28.51 31.90 29.09 30.86 30.41 29.09 29.84 30.05 30.81 Rb 168.92 170.11 165.97 172.04 176.44 168.76 171.70 172.47 162.74 172.63 186.60 169.82 168.03 167.27 164.24 170.68 Cs 2.73 3.69 3.50 2.46 2.62 3.03 3.53 2.89 4.11 3.03 5.94 3.74 3.76 4.65 3.18 2.63 Sr 74.37 76.06 78.41 37.44 48.73 38.32 49.51 39.40 78.47 77.74 83.05 80.12 79.08 79.44 85.69 54.51 Sc 6.38 6.35 6.22 3.76 3.75 3.70 4.17 3.68 5.39 5.64 5.74 5.25 6.21 6.14 6.27 5.94 Zr 374.17 366.69 384.62 263.06 283.65 232.20 266.84 230.83 318.32 369.69 372.26 360.45 362.82 372.39 384.12 296.26

333 Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Member Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin

Canyon Canyon Canyon Canyon Canyon Canyon Flow - Flow - Flow - Canyon Canyon Canyon Canyon Canyon Canyon Flow - Flow - Canyon Canyon Canyon Canyon Unit Flow upper middle middle Flow Flow Flow Flow Flow Flow? basal basal Flow Flow Flow Flow?

just off of top of flow top 7-mile hole Wapiti Wapiti Wapiti S. Side of 7-mile hole N. Canyon 7-mile hole canyon? Canyon Wapiti Wapiti flow top flow top flow top breccia? Locality trail Lake Trail Lake Trail Lake Trail Canyon trail rim trail DRF? Flow? Lake Trail Lake Trail breccia breccia breccia Near DRF northing 4954608 4949631 4949650 4949632 4951779 4952902 4953840 4952962 4954402 4955445 4949539 4949551 4951788 4951788 4951788 4955140 easting (12) 543767 555899 555943 555944 542020 542534 544277 542596 542025 542567 555886 555907 542030 542030 542030 542797 Lithology wx tuff vitric-tuff tuff tuff wx glass wx glass wx glass wx glass vitric vitric vitric vitric breccia pumice breccia breccia Source CJP09 CJP09 CJP09 CJP09 CJP 09 CJP08 CJP08 CJP08 CJP09 CJP09 CJP09 CJP09 CJP 08 CJP 08 CJP 08 CJP09 Age (Ma) 0.484 0-Jan-00 0-Jan-00 0-Jan-00 0.484 0.484 0.484 0.484 0.484 0.484 0.484 0-Jan-00 0.484 0.484 0.484 0.484 Age error 0.015 0.02 0.02 0.02 0.015 0.015 0.015 0.015 0.015 0.015 0.015 0.02 0.015 0.015 0.015 0.015 Sample # 0923 0935B 0936 0937 08CP24 08CP38 08CP42 08CP44 0915 0920 0933 0934 08CP25A 08CP25B 08CP25C 0926 Date 9/6/2009 9/6/2009 9/6/2009 9/6/2009 12/29/2008 1/2/2009 1/2/2009 1/2/2009 9/6/2009 9/6/2009 9/6/2009 9/6/2009 12/29/2008 12/29/2008 12/29/2008 9/6/2009 SiO2 75.99 76.07 75.74 75.40 76.23 76.15 75.96 76.17 76.43 74.75 74.57 75.01 80.06 77.90 77.09 75.62 TiO2 0.34 0.34 0.35 0.37 0.34 0.35 0.35 0.36 0.28 0.40 0.39 0.36 0.31 0.33 0.32 0.37 Al2O3 12.51 12.73 12.87 12.86 12.86 13.10 12.51 13.23 12.52 12.82 13.33 12.88 11.35 12.57 12.39 12.80 FeO* 2.16 1.41 1.55 1.83 1.65 2.04 1.91 2.03 1.52 2.43 2.02 2.11 1.15 1.35 1.28 2.25 MnO 0.02 0.05 0.07 0.05 0.03 0.04 0.04 0.04 0.03 0.09 0.06 0.06 0.04 0.04 0.04 0.05 MgO 0.08 0.14 0.14 0.13 0.08 0.07 0.07 0.04 0.09 0.25 0.24 0.23 0.10 0.08 0.08 0.08 CaO 0.65 0.89 0.94 1.00 0.85 0.82 0.79 0.64 0.67 1.17 1.29 1.15 0.88 0.89 0.82 0.95 Na2O 3.28 3.55 3.56 3.64 2.39 2.00 2.96 2.48 3.51 3.40 3.57 3.49 1.74 1.78 2.08 2.76 K2O 4.93 4.80 4.74 4.67 5.55 5.40 5.37 4.98 4.90 4.63 4.47 4.68 4.36 5.02 5.88 5.08 P2O5 0.04 0.04 0.04 0.05 0.03 0.03 0.04 0.02 0.03 0.05 0.06 0.05 0.03 0.03 0.02 0.05 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 96.63 97.33 97.60 97.87 95.48 94.62 96.26 94.86 97.66 96.15 94.83 95.78 94.44 93.90 95.11 94.43 T.A. 8.21 8.34 8.30 8.31 7.94 7.40 8.33 7.47 8.42 8.03 8.04 8.17 6.10 6.81 7.96 7.84

XRF (ppm) Ni 2.00 2.10 0.70 1.70 0.00 1.38 0.90 0.15 2.30 4.30 1.80 4.40 0.00 0.00 0.00 2.40 Cr 2.80 3.10 5.60 4.50 3.10 2.80 3.70 2.40 3.30 3.50 4.90 4.40 3.10 4.10 3.90 3.40 Sc 6.00 5.20 6.10 6.00 6.40 6.40 5.90 5.40 4.20 5.90 6.40 6.00 5.10 5.40 5.00 5.80 V 4.10 6.20 5.50 3.50 5.20 4.50 4.10 2.20 4.00 7.00 6.90 5.50 2.70 1.70 1.10 6.10 Ba 972.30 1058.10 1119.10 1141.90 1028.40 984.20 1001.50 932.80 928.60 1106.70 1191.20 1076.50 938.10 1037.80 994.10 1035.90 Rb 171.10 159.70 157.30 152.40 195.60 178.70 182.50 165.90 167.10 158.60 143.80 153.80 181.10 208.90 197.60 168.20 Sr 70.30 87.20 102.40 105.40 86.80 77.00 75.00 68.00 62.60 106.20 125.10 100.00 92.40 87.60 73.70 86.70 Zr 379.60 384.60 378.40 404.10 372.90 369.80 366.90 381.30 326.40 431.00 409.90 377.30 328.00 345.50 348.80 398.20 Y 68.30 57.00 59.20 74.30 63.70 166.20 63.90 59.70 64.80 62.30 61.10 62.20 54.80 59.10 62.70 65.20 Nb 48.40 47.80 46.70 46.60 47.20 49.00 48.00 49.20 46.40 45.30 43.70 46.20 41.70 46.10 48.10 47.00 Ga 20.00 21.20 20.10 21.50 20.90 20.50 19.70 20.90 20.60 20.80 19.90 20.40 17.50 19.10 19.60 19.50 Cu 1.30 1.00 1.40 1.60 0.00 0.60 0.00 1.90 0.10 3.20 1.80 1.20 0.20 0.00 0.60 0.80 Zn 63.60 60.30 73.10 92.90 74.70 76.50 78.80 70.10 50.50 88.30 72.40 75.30 63.10 55.20 55.50 68.60 Pb 26.30 31.10 31.60 30.50 31.20 30.40 30.10 31.10 29.90 30.20 28.50 29.90 28.50 30.10 30.40 30.00 La 81.80 76.50 72.70 80.00 77.60 80.60 77.70 78.50 79.00 72.90 74.00 75.10 68.40 69.90 73.20 75.10 Ce 156.40 142.60 143.50 157.60 147.20 157.80 151.20 148.20 146.20 141.00 142.90 143.60 125.50 139.40 140.40 147.40 Th 23.60 23.40 22.10 21.90 24.00 25.10 23.80 26.40 23.60 22.60 21.20 22.00 21.20 22.90 25.40 23.20 Nd 63.90 55.20 58.40 66.60 58.20 75.90 61.00 58.90 61.40 58.00 56.00 59.50 50.70 54.90 56.10 60.00 U 4.90 7.20 5.80 4.80 5.70 6.10 6.20 4.90 6.40 6.30 4.90 4.70 4.10 5.20 5.20 5.70 6.30 4.30 3.70 0.20 3.50 3.10 5.50 3.70 2.70 ICP-MS (ppm) La 82.72 76.27 75.70 83.77 77.91 84.58 81.52 80.34 81.14 76.51 75.60 75.40 69.01 73.28 76.56 77.57 Ce 157.54 144.96 148.46 160.70 148.30 168.88 156.87 152.94 149.60 147.86 145.65 144.60 128.48 141.46 146.34 149.71 Pr 18.46 16.41 16.52 18.81 16.84 20.34 17.94 17.15 17.75 16.59 16.38 16.41 14.72 15.90 16.51 17.07 Nd 67.15 58.83 60.19 70.46 60.82 81.10 65.20 61.31 64.62 61.19 59.50 59.78 52.73 57.91 59.86 62.25 Sm 13.83 11.88 12.36 14.73 12.42 19.48 13.36 12.36 13.05 12.61 12.18 12.25 10.62 11.92 12.27 12.86 Eu 1.89 2.04 2.22 2.48 1.97 4.27 1.89 1.70 1.67 2.32 2.56 2.22 1.78 1.92 1.84 2.04 Gd 12.91 10.66 11.19 13.91 11.45 24.23 12.04 11.17 11.75 11.57 11.39 11.15 9.73 10.91 11.09 11.90 Tb 2.18 1.83 1.91 2.37 1.95 4.24 2.07 1.87 2.01 1.96 1.91 1.92 1.64 1.86 1.92 2.02 Cy 13.22 11.06 11.61 14.33 11.98 26.62 12.49 11.50 12.24 11.82 11.58 11.76 10.13 11.21 11.87 12.22 Ho 2.61 2.24 2.30 2.91 2.45 5.68 2.51 2.33 2.40 2.39 2.34 2.35 2.09 2.25 2.39 2.48 Er 7.04 6.09 6.27 7.94 6.77 15.41 6.83 6.37 6.53 6.47 6.30 6.45 5.74 6.31 6.56 6.73 Tm 1.01 0.89 0.91 1.14 1.00 2.13 0.98 0.94 0.95 0.95 0.92 0.93 0.85 0.93 0.97 0.99 Yb 6.26 5.58 5.70 7.10 6.15 12.26 6.08 5.83 5.79 5.87 5.66 5.78 5.28 5.74 6.01 6.09 Lu 0.93 0.84 0.86 1.09 0.95 1.87 0.93 0.89 0.87 0.89 0.86 0.89 0.80 0.88 0.93 0.93 Ba 1001.48 1079.81 1144.38 1180.96 1047.04 1022.52 1035.38 967.68 946.86 1146.58 1237.09 1105.73 970.35 1067.36 1017.02 1066.48 Th 23.72 23.38 22.44 22.17 23.02 24.49 23.96 24.89 23.39 21.52 21.09 22.08 19.98 22.82 23.41 22.94 Nb 48.70 48.04 46.50 46.95 47.89 49.99 49.39 50.69 46.75 46.31 44.94 46.76 42.56 46.95 47.52 47.58 Y 66.49 54.58 56.83 71.36 63.25 167.92 64.51 59.81 62.45 60.86 59.49 60.72 53.53 58.99 61.77 64.03 Hf 10.63 11.04 10.90 11.51 10.68 10.87 10.95 11.38 9.67 11.73 11.44 10.68 9.53 10.25 10.41 11.26 Ta 3.44 3.39 3.27 3.24 3.34 3.47 3.41 3.54 3.23 3.16 3.11 3.25 2.93 3.30 3.33 3.31 U 5.33 5.87 5.59 5.57 5.69 6.46 5.96 5.93 5.83 5.32 5.34 5.40 4.61 5.36 5.79 5.70 Pb 26.91 30.92 30.39 29.46 30.61 31.91 31.06 32.01 29.51 30.05 28.45 29.06 28.16 30.24 30.65 30.84 Rb 174.96 159.69 158.88 154.53 202.72 184.52 186.33 171.08 167.54 157.14 147.76 156.19 188.93 219.94 204.97 171.23 Cs 3.80 3.66 3.19 3.10 6.81 4.44 5.15 4.35 3.13 3.39 3.81 3.78 12.53 9.39 5.40 5.01 Sr 72.00 86.50 101.89 105.23 88.78 79.53 76.95 69.54 62.73 105.87 125.91 101.19 93.98 91.05 75.50 88.18 Sc 5.90 6.17 6.70 6.92 5.64 6.51 6.29 5.70 5.29 7.28 7.33 7.18 5.48 5.14 5.02 6.92 Zr 372.72 393.79 389.12 416.66 366.56 373.21 373.64 386.13 331.86 435.05 426.81 388.98 329.98 351.51 354.07 403.36

334 Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Upper Member Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin Basin

Canyon Flow - Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Dunraven Unit upper Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow Road Flow

West stoney portion on interior Wapiti Dunraven Dunraven top of ring southern from ring Locality Lake Trail Pass Pass fracture hill - fracture northing 4949631 4955387 4955387 4955840 4955321 4954982 4954966 4956314 4955406 4954729 4955445 4955491 4956017 4955642 easting (12) 555899 540434 540434 542283 542127 542321 542541 542310 541714 542576 542131 542200 542455 542334 Lithology volcanic sed.picked glass vitric obsidian vitric obsidian wx obsidiannded obsidi wx glass vitrophyre wx tuff tuff tuff tuff Source CJP09 CJP 07 CJP 07 CJP 08 CJP 08 CJP 08 CJP 08 CJP 08 CJP09 CJP09 CJP 08 CJP 08 CJP 08 CJP09 Age (Ma) 0-Jan-00 0.486 0.486 0.486 0.486 0.486 0.486 0.486 0.486 0.486 0.486 0.486 0.486 0.486 Age error 0.02 0.042 0.042 0.042 0.042 0.042 0.042 0.042 0.042 0.042 0.042 0.042 0.042 0.042 Sample # 0935A 07CP15-OBS 07CP15 08CP01 08CP03 08CP04 08CP05 08CP09 0908 0919 08CP02 08CP07 08CP08 0921 Date 9/6/2009 16-Jan-10 19-Dec-07 27-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 28-Dec-08 5-Sep-09 6-Sep-09 27-Dec-08 28-Dec-08 28-Dec-08 6-Sep-09 SiO2 73.98 77.46 77.59 77.34 77.54 77.53 76.87 77.44 77.24 77.50 77.62 77.74 77.52 77.57 TiO2 0.45 0.138 0.125 0.126 0.121 0.120 0.156 0.118 0.122 0.117 0.122 0.121 0.119 0.118 Al2O3 13.97 11.87 12.17 12.09 12.07 11.99 12.56 12.06 12.28 12.01 12.22 12.09 12.16 12.10 FeO* 1.68 1.26 0.88 1.18 1.23 1.12 1.30 1.13 1.17 1.17 1.01 0.99 1.11 1.22 MnO 0.05 0.034 0.023 0.032 0.017 0.031 0.029 0.031 0.032 0.032 0.007 0.014 0.019 0.013 MgO 0.28 0.11 0.04 0.07 0.03 0.05 0.06 0.05 0.05 0.04 0.03 0.02 0.03 0.01 CaO 1.54 0.56 0.47 0.53 0.35 0.48 0.51 0.50 0.49 0.50 0.36 0.34 0.37 0.37 Na2O 3.80 3.15 3.48 3.49 3.45 3.47 3.40 3.49 3.47 3.47 3.45 3.47 3.49 3.44 K2O 4.20 5.40 5.20 5.13 5.18 5.17 5.09 5.16 5.12 5.15 5.17 5.19 5.17 5.15 P2O5 0.07 0.018 0.017 0.014 0.015 0.012 0.019 0.012 0.015 0.012 0.017 0.023 0.016 0.013 Total 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 100.00 Raw Sum 97.50 99.81 96.73 98.88 99.81 99.09 98.53 99.48 97.91 97.84 99.51 99.67 100.26 97.55 T.A. 7.99 8.55 8.68 8.62 8.64 8.65 8.50 8.66 8.60 8.62 8.61 8.66 8.66 8.59

XRF (ppm) Ni 3.20 4 0 0 3 1 0 0 4 2 1 1 2 3 Cr 10.00 4 2 4 2 2 3 3 3 3 4 3 2 3 Sc 8.40 4 3 4 3 5 4 4 4 5 4 3 4 3 V 13.20 4 -1 2 1 2 2 1 3 2 1 0 2 1 Ba 1360.40 635 654 654 675 659 715 663 655 643 658 668 666 657 Rb 123.90 184 169 168 169 171 166 170 170 166 170 170 170 164 Sr 173.00 16 19 20 20 17 29 19 20 18 19 20 20 18 Zr 441.10 196 187 186 192 187 212 187 194 191 188 188 190 190 Y 45.20 54 48 52 43 52 48 53 53 53 45 47 47 28 Nb 41.90 35.4 33.9 33.3 34.4 33.1 36.1 33.3 33.0 34.1 33.8 34.7 33.7 33.3 Ga 22.60 19 21 19 19 18 21 19 20 20 19 20 19 20 Cu 4.00 5 -1 0 0 0 0 0 0 0 0 0 0 2 Zn 60.90 51 41 51 41 51 51 52 48 50 33 36 50 46 Pb 27.80 33 34 31 30 30 31 34 32 31 27 26 38 30 La 65.10 60 58 60 50 61 59 63 62 60 55 65 53 36 Ce 128.80 124 109 117 118 119 122 120 118 117 93 170 109 69 Th 19.30 21 24 21 21 21 21 21 21 20 22 22 22 20 Nd 48.90 49 45 46 38 46 45 47 50 46 43 55 41 25 U 5.20 4 4 5 4 5 5 4 6 4 3 5 5 5 0.90 ICP-MS (ppm) La 66.04 62.21 60.39 62.52 49.46 62.23 63.24 62.58 65.64 62.98 55.30 68.52 56.51 37.26 Ce 130.94 119.22 111.95 119.12 120.71 119.52 120.82 119.97 125.69 119.96 91.75 170.32 112.64 72.50 Pr 13.96 13.45 12.80 13.39 11.10 13.42 13.08 13.53 14.21 13.51 12.56 16.01 12.08 7.66 Nd 50.26 48.29 45.68 48.38 39.61 48.38 46.64 48.53 51.21 48.76 44.76 58.24 42.82 26.93 Sm 10.02 10.15 9.49 10.15 8.53 10.09 9.57 10.13 10.67 10.18 9.57 12.25 8.91 5.72 Eu 2.90 0.66 0.69 0.72 0.68 0.69 0.85 0.70 0.74 0.72 0.73 0.74 0.71 0.69 Gd 8.76 9.36 8.78 9.32 7.30 9.15 8.65 9.21 9.61 9.35 8.24 10.50 7.86 5.11 Tb 1.45 1.60 1.50 1.58 1.29 1.59 1.49 1.59 1.65 1.61 1.43 1.75 1.42 0.93 Cy 8.75 9.80 9.19 9.71 8.11 9.77 9.19 9.88 9.89 9.89 8.75 10.36 9.10 5.70 Ho 1.73 1.96 1.82 1.95 1.60 1.96 1.83 1.97 1.95 1.97 1.73 1.87 1.84 1.16 Er 4.72 5.30 4.92 5.33 4.44 5.35 4.91 5.30 5.23 5.34 4.72 4.85 5.03 3.21 Tm 0.70 0.77 0.72 0.76 0.67 0.78 0.72 0.78 0.76 0.77 0.68 0.70 0.74 0.49 Yb 4.41 4.73 4.35 4.77 4.32 4.80 4.44 4.73 4.67 4.80 4.27 4.28 4.66 3.11 Lu 0.68 0.72 0.66 0.72 0.66 0.72 0.68 0.72 0.69 0.73 0.63 0.61 0.69 0.46 Ba 1394.26 643 671 664 678 657 725 665 677 666 671 674 672 656 Th 18.96 20.36 23.07 20.14 21.17 20.55 21.28 20.41 20.81 20.34 20.69 21.34 20.63 20.39 Nb 41.94 33.33 34.24 33.45 33.41 32.74 35.47 33.22 33.62 33.83 33.02 33.85 31.99 33.75 Y 43.80 50.33 47.02 51.20 41.11 50.89 46.07 51.12 50.58 51.24 44.69 45.72 44.92 27.03 Hf 11.72 6.97 7.06 7.06 6.98 6.93 7.61 7.05 7.08 6.91 7.07 6.95 7.10 6.79 Ta 2.80 2.49 2.54 2.50 2.51 2.46 2.65 2.49 2.48 2.46 2.53 2.50 2.42 2.50 U 4.75 4.68 4.67 4.53 4.38 4.59 4.75 4.62 4.57 4.54 4.08 4.47 4.78 4.35 Pb 26.82 30.98 32.10 31.44 29.96 31.13 31.60 33.60 31.94 31.44 27.29 26.14 38.17 28.49 Rb 123.79 185.9 172.4 172.2 168.2 170.0 165.5 171.1 170.1 167.4 170.3 171.3 171.1 167.3 Cs 3.08 3.41 3.27 3.38 2.31 3.40 3.65 3.41 3.44 3.40 2.27 2.84 2.57 1.84 Sr 168.17 15.47 19.28 20.14 19.96 17.42 27.77 18.88 21 18 19.35 19.59 19.08 20 Sc 8.55 3.70 3.44 4.00 3.50 3.75 3.94 3.98 4.7 4.7 3.83 3.58 4.60 3.9 Zr 447.07 187 192 191 191 187 213 189 201 197 190 191 190 195

335

APPENDIX N

RESOURCES FOR CHAPTER 3 – OXYGEN ISOTOPE RATIOS FROM THE EUBM

Tuff of Sulphur Creek Caynon Flow Dunraven Road Flow 18 18 18 SAMPLE TYPE δ O VSMOW SAMPLE TYPE δ O VSMOW SAMPLE TYPE δ O VSMOW 07-CP-01 quartz 1.539 08CP26.2 quartz 2.911 08CP01.1 plag 3.630 07-CP-01 quartz 2.4 08CP26.1 quartz 2.287 08CP01.2 plag 5.695 07-CP-03 quartz 1.691 0920.1 quartz 2.429 08CP01.3 plag 3.480 07-CP-04 quartz 1.896 0920.2 quartz 2.489 08CP01.4 plag 3.530 07-CP-09 quartz 1.893 0934 quartz 3.872 08CP03.1 plag 3.571 07-CP-09 quartz 1.773 0934 quartz 4.61 08CP07.1 plag 4.136 07-CP-10 quartz 2.103 08CP26.2 plag 0.880 08CP02.2 plag 4.7985 07-CP-10 quartz 1.873 0920.4 plag 0.9705 08CP02.3 plag 3.7595 07-CP-12 quartz 1.751 0934 plag 0.80 08CP02.4 plag 2.588 07-CP-12 quartz 1.936 08CP26.1 a. felds 1.832 07-CP-03 plagioclase 0.32 0920.3 a. felds 1.7465 QUARTZ - vapor phase 07-CP-04 plagioclase 0.299 0934 a. felds 2.74 08CP02.1 quartz 1.876 07-CP-12 plagioclase 0.32 0934 CPX 0.66 08CP07.2 quartz 1.202 07-CP-12 plagioclase 0.284 07-CP-01 plagioclase 0.4

Tuff of sulphur Creek Pumice 18 SAMPLE TYPE δ O VSMOW 08CP28.1 quartz 2.446 08CP28.2 quartz 2.324

337

APPENDIX O

RESOURCES FOR CHAPTER 3 – LASER ABLATION OF PLACIOGLCASE, 87SR/86SR FROM THE EUBM

Corrected run # run name slide# 87Sr/86Sr ERROR core/ rim Unit 1 G1.1 7-12 0.716700836 0.000197 core small Tuff of Sulphur Creek 2 G2.1 7-12 0.716610901 0.000192 core Tuff of Sulphur Creek 3 G3.1 7-12 0.716251162 0.000183 core Tuff of Sulphur Creek 4 G3.2 7-12 0.716291133 0.000197 rim Tuff of Sulphur Creek 5 G2.2 7-12 0.717061884 0.000130 rim Tuff of Sulphur Creek 6 G4.1 7-12 0.716622428 0.000184 rim Tuff of Sulphur Creek 7 G4.2 7-12 0.717211699 0.000139 core Tuff of Sulphur Creek 9 G6.1 7-12 0.7172916 0.000139 core Tuff of Sulphur Creek 10 G7.1 7-12 0.717381488 0.000156 core small Tuff of Sulphur Creek 11 G8.1 7-12 0.717301587 0.000139 core Tuff of Sulphur Creek 12 G8.2 7-12 0.718110585 0.000147 rim Tuff of Sulphur Creek 13 G8.3 7-12 0.717940796 0.000147 rim Tuff of Sulphur Creek 14 G9.1 7-12 0.717031921 0.000139 core Tuff of Sulphur Creek 15 G9.2 7-12 0.717661142 0.000129 rim Tuff of Sulphur Creek 16 G10.1 7-12 0.716133035 0.000122 core Tuff of Sulphur Creek 17 G11.1 0835 0.715214173 0.000106 core Tuff of Sulphur Creek 18 G11.2 0835 0.715114296 0.000092 rim Tuff of Sulphur Creek 19 G12.1 0835 0.717201711 0.000130 core small Tuff of Sulphur Creek 20 G13.1 0835 0.717371501 0.000122 core Tuff of Sulphur Creek 21 G13.2 0835 0.71750134 0.000122 rim Tuff of Sulphur Creek 22 G14.1 0835 0.715543764 0.000099 core small Tuff of Sulphur Creek 23 G14.2 0835 0.715713554 0.000106 rim small Tuff of Sulphur Creek 24 G15.1 0835 0.715473851 0.000114 core small Tuff of Sulphur Creek 25 G16.1 0835 0.715763492 0.000114 rim Tuff of Sulphur Creek 26 G16.2 0835 0.715933282 0.000122 core Tuff of Sulphur Creek 27 G17.1 0835 0.717271624 0.000130 core Tuff of Sulphur Creek 28 G18.1 0835 0.716542527 0.000130 rim Tuff of Sulphur Creek 29 G19.1 0835 0.71847014 0.000495 core Tuff of Sulphur Creek 30 G20.1 0835 0.715403938 0.000106 core small Tuff of Sulphur Creek 31 G21 0801 0.713586189 0.000221 core small Dunraven Road flow 32 G22 0801 0.714065595 0.000193 core small Dunraven Road flow 33 G23.1 0801 0.714055608 0.000202 rim Dunraven Road flow 34 G23.2 0801 0.713736003 0.000212 core Dunraven Road flow 36 G25 0801 0.714055608 0.000231 core Dunraven Road flow 37 G26 0801 0.714015657 0.000202 core Dunraven Road flow 38 G27 0801 0.714405175 0.000212 core Dunraven Road flow 39 G28 0801 0.714405175 0.000212 core Dunraven Road flow 40 G29 0801 0.713356473 0.000212 core Dunraven Road flow 41 G30.1 0801 0.713536251 0.000212 core Dunraven Road flow 42 G30.2 0801 0.713765966 0.000174 rim Dunraven Road flow 43 G31.1 0934 0.716292837 0.000114 rim Canyon flow 44 G31.2 0934 0.716372738 0.000114 rim Canyon flow 45 G31.3 0934 0.716023171 0.000114 core Canyon flow 46 G31.4 0934 0.715883344 0.000122 core Canyon flow 48 G33.1 0934 0.717981745 0.000147 core Canyon flow 49 G33.2 0934 0.717521315 0.000130 rim Canyon flow 50 G34 0934 0.716942033 0.000122 core small Canyon flow 51 G35 0934 0.715383962 0.000174 core Canyon flow 52 G36 0934 0.717271624 0.000114 core Canyon flow 53 G37 0934 0.716602453 0.000130 core small Canyon flow 54 G38 0934 0.716892094 0.000147 core small Canyon flow 55 G39 0934 0.716252886 0.000130 core Canyon flow 56 G40 0934 0.716392713 0.000130 core Canyon flow 57 G41.1 0934 0.716872119 0.000130 rim Canyon flow 58 G41.2 0934 0.716682354 0.000114 core Canyon flow

339