4. Final Report Hard Aggregate Study

Total Page:16

File Type:pdf, Size:1020Kb

4. Final Report Hard Aggregate Study ALASKA DEPARTMENT of TRANSPORTATION and PUBLIC FACILITIES STATEWIDE MATERIAL SITE INVENTORY, SITE INSPECTIONS & GEOLOGICAL INVESTIGATIONS HARD AGGREGATE SOURCE LOCATION STUDY FEDERAL PROJECT NO. STP-000S(823) AKSAS PROJECT NO. 76149 Prepared by: R&M CONSULTANTS, INC. 9101 Vanguard Drive Anchorage, Alaska 99507 STATE OF ALASKA DOT&PF STATEWIDE MATERIAL SITE INVENTORY, SITE INSPECTIONS & GEOLOGICAL INVESTIGATIONS HARD AGGREGATE SOURCE LOCATION STUDY FEDERAL PROJECT NO. STP-000S(823) AKSAS PROJECT NO. 76149 ALASKA DEPARTMENT OF TRANSPORTATION & PUBLIC FACILITIES 5800 East Tudor Road Anchorage, Alaska 99507-1286 Prepared by: R&M CONSULTANTS, INC. 9101 Vanguard Drive Anchorage, Alaska 99507 May, 2013 NOTE TO READERS This Hard Aggregate Source Location Study has been prepared to provide useful information to multiple groups of readers, including executive decision-makers, geologists, engineers and planners, and materials end-users. As such, it contains information that may be highly useful to one group, yet too detailed or too broad for the next. The following guidelines are intended to help each group of readers quickly find the information that will be most useful to them. Executive decision-makers will perhaps be most interested in the Executive Summary, the Conclusions (Chapter 7.0), the appended source reports, and the attached plate. Based on available time and interest, this group of readers may also glean useful information from Chapters 1.0 through 3.0. Geologists will find the entire study to be of use. Depending on what their immediate need or interest may be, this group of readers may choose to focus on a particular region or area of study, or on a particular hard aggregate source. Before focusing on a geographic area, however, the geologist reader will be well served by reading Chapters 1.0 through 3.0. This group of readers will also find Chapters 4.0 through 6.0 to be condensed treatments of a broad cross section of geological areas; as such, these latter chapters will provide useful reference material. This group of readers will be able to utilize this study as a starting point for prospecting and planning the development of hard aggregate sources. Engineers and planners will likely wish to focus on the Executive Summary, Conclusions (Chapter 7.0), and the two attached Plates. For project-specific or area-specific interests, this group of readers will also find utility in the appended source reports. Prior to using the information herein, engineers and planners will wish to become familiar with Chapters 1.0 and 2.0, with at least a cursory review of Chapter 3.0. Materials end-users will be most interested in the appended source reports. Next in importance for this group of readers will be the Executive Summary and Conclusions (Chapter 7.0), followed by Chapters 1.0 through 3.0. Statewide Material Site Inventory Hard Aggregate Location Study i Final Report STATE OF ALASKA DOT&PF STATEWIDE MATERIAL SITE INVENTORY, SITE INSPECTIONS & GEOLOGICAL INVESTIGATIONS HARD AGGREGATE SOURCE LOCATION STUDY TABLE OF CONTENTS Page NOTE TO READERS ..................................................................................................................... i TABLE OF CONTENTS ................................................................................................................ ii LIST OF TABLES ......................................................................................................................... iii LIST OF FIGURES ....................................................................................................................... iv LIST OF APPENDICES ..................................................................................................................v EXECUTIVE SUMMARY ........................................................................................................... vi 1.0 INTRODUCTION ...............................................................................................................1 1.1 Background ..............................................................................................................1 1.2 Scope-of-Work .........................................................................................................5 1.3 Assumptions .............................................................................................................6 1.4 Contract Authorization.............................................................................................6 2.0 AGGREGATE / ROCK TESTING .....................................................................................7 2.1 Los Angeles Abrasion (ASTM C 131) ....................................................................7 2.2 Degradation Value of Aggregates (ATM 313) ........................................................8 2.3 Specific Gravity and Absorption (ASTM C 128) ....................................................8 2.4 Unconfined Compressive Strength (ASTM D 7012) ...............................................8 3.0 GEOLOGY OF HARD AGGREGATES ..........................................................................10 3.1 General ...................................................................................................................10 3.2 Weathering .............................................................................................................10 3.3 Origin and Type of Rock .......................................................................................11 3.3.1 Sedimentary Rocks .................................................................................... 14 3.3.2 Igneous and Volcanic Rocks ..................................................................... 14 3.3.3 Metamorphic Rocks .................................................................................. 14 3.3.3.1 Hornfels ............................................................................................... 15 3.3.3.2 Quartzite and Gneiss ........................................................................... 16 3.3.3.3 Greenstone ........................................................................................... 16 3.3.4 Unconsolidated Material ........................................................................ 17 3.4 Porosity, Grain-Size, and Grain Shape ..................................................................17 3.5 Selected References ...............................................................................................19 4.0 SOUTHCENTRAL ALASKA...........................................................................................20 4.1 General Geology ....................................................................................................20 4.2 Kenai Peninsula .....................................................................................................20 4.3 Seldovia Area .........................................................................................................23 4.4 West Chugach Mountains – Anchorage to Eklutna ...............................................24 Statewide Material Site Inventory Hard Aggregate Location Study ii Final Report 4.5 East-Central Chugach Mountains – Knik/Matanuska ............................................27 4.6 Western Talkeetna Mountains ...............................................................................30 4.7 Petersville Road .....................................................................................................33 4.8 Southern Talkeetna Mountains ..............................................................................33 4.9 Prince William Sound ............................................................................................35 4.10 Selected References ...............................................................................................46 5.0 ALASKA PENINSULA, ALEUTIAN ISLANDS, AND KODIAK ISLAND .................49 5.1 General Geology ....................................................................................................49 5.2 Unalaska .................................................................................................................49 5.3 False Pass, Cold Bay and King Cove.....................................................................54 5.4 Sand Point and Shumagin Islands ..........................................................................54 5.5 Perryville ................................................................................................................56 5.6 Chignik ...................................................................................................................57 5.7 Kamishak Bay to Iliamna Bay ...............................................................................57 5.8 Kodiak Island .........................................................................................................59 5.9 Selected References ...............................................................................................60 6.0 SOUTHEAST ALASKA ...................................................................................................62 6.1 General Geology ....................................................................................................62 6.2 Skagway Area ........................................................................................................64 6.3 Haines Highway Area ............................................................................................65 6.4 Juneau and Admiralty Island
Recommended publications
  • Or Early Callovian) Ammonites from Alaska and Montana
    Jurassic (Bathonian or Early Callovian) Ammonites From Alaska and Montana By RALPH W. IMLAY SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 374-C Descr$tions and illustrations of ctphalopods of possible late Middle Jurasric (Bathonian) age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page C- 1 Age of the faunas-Continued C- 1 Callovian versus Bathonian in Greenland- - - - _ - - _ - - C-2 Callovian versus Bathonian in Alaska and Montana- -- - Stratigraphic summary- __ --______ _ - - - -- - ---.- -- -.- - - C-2 Paleogeographic considerations- - -_-- -- ---- ---- Cook Inlet region, Alaska -______--------.-.--..--c-2 Summation of the evidence- - - _._ _ - _ _ - - - - - - - - - - - - Iniskin Peninsula-_-_______----.--------~.--C-2 Comparisons with other faunas---------___----------- Peninsula north of Chinitna Bay----- __._ _ _._ - C-3 \Vestern interior of Canada- - - -- -- -____------- --- Talkeetna Mountains ----___-_ - - -- ---- - - -- - -- C-3 Arctic region-_-_---___-_----------------------- Western Montana- - -----__-----------------.---C-5 other regions--__-__-____----------------------- Rocky Mountain front north of the Sun River- (2-5 Geographic distribution ___-___ --- - ---------- ------ -- - Drummond area--- ---_____ _--- -- -.-- ---- -- - C-10 Summary of results- --_-____-_----_---_-_----------- Age ofthe faunas-----------_----------------------- GI0 Systematic descriptions--_ _ _ - _ - - - - - - - - - - - - - - - - - - - - - - - Evidence from Alaska---____________--------------C-10 Literature cited _-_-_---______----------------------- Evidence from Montana --_-_____ --- - - -- .--- --- - - C-12 Index---__--___-_-_------------------------------- ILLUSTRATIONS [Plates 1-3 follow index] PLATE 1. Holcophylloceras, Oecotraustes (Paroecotraustes) ?, and Arctocephalites (Cranocephalites). 2.
    [Show full text]
  • 1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
    https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing.
    [Show full text]
  • THE CITY and BOROUGH of JUNEAU, ALASKA Petition for the Annexation of Approximately 1977 Square Miles Using the Local-Option
    THE CITY AND BOROUGH OF JUNEAU, ALASKA Petition for the Annexation of Approximately 1977 Square Miles Using the Local-Option Method (3 AAC 110.210(3)) Volume I of IV (Sections 1 – 21; Exhibits A – K) Submitted to: The Local Boundary Commission March 13, 2012 TABLE OF CONTENTS Section 1. Name of Petitioner ………………………………………………………… 1 Section 2: Petitioner’s Representative ………………………………………………... 1 Section 3: Name and Class of the Organized Borough ……………………………….. 1 Section 4: General Description of the Nature of the Proposed Action ……………….. 2 Section 5: General Description of the Area Proposed for Annexation ……………….. 2 Section 6: Statement of Reason for Annexation ……………………………………… 2 Section 7: Legal Description and Maps ………………………………………………. 3 Section 8: Size ………………………………………………………………………... 3 Section 9: Population …………………………………………………………………. 4 Section 10: Information Relating to Public Notice …………………………………… 4 Section 11: Tax Data ………………………………………………………………….. 4 A. Value of Taxable Property in the Area Proposed for Annexation …… 4 B. Projected Taxable Sales in the Area Proposed for Annexation ……… 4 C: Municipal Government Tax Levy Currently in Effect ………………. 5 i. Taxes Currently Levied by CBJ ………………………………. 5 ii. Taxes Currently Levied in Annexation Area …………………. 5 Section 12: Projected Revenue, Operating Expenditures, and Capital Expenditures … 5 Section 13: Existing Long-Term Municipal Debt ……………………………………. 12 Section 14: Powers and Services ……………………………………………………... 13 A. Current Borough Powers and Functions ……………………………... 13 B. Post-Annexation Services and Functions …………………………….. 13 C. Alternative Service Providers ………………………………………… 13 Section 15: Transition Plan …………………………………………………………… 13 Section 16: Federal Voting Rights Act Information …………………………………. 14 Section 17: Composition and Apportionment of Assembly …………………………. 14 Section 18: Supporting Legal Brief …..………………………………………………. 14 Section 19: Authorization …………………………………………………………….. 14 Section 20: Affidavit of Accuracy ……………………………………………………. 14 Section 21: Other Information ……………………………………………………….
    [Show full text]
  • Wilderness in Southeastern Alaska: a History
    Wilderness in Southeastern Alaska: A History John Sisk Today, Southeastern Alaska (Southeast) is well known remoteness make it wild in the most definitive sense. as a place of great scenic beauty, abundant wildlife and The Tongass encompasses 109 inventoried roadless fisheries, and coastal wilderness. Vast expanses of areas covering 9.6 million acres (3.9 million hectares), wild, generally undeveloped rainforest and productive and Congress has designated 5.8 million acres (2.3 coastal ecosystems are the foundation of the region’s million hectares) of wilderness in the nation’s largest abundance (Fig 1). To many Southeast Alaskans, (16.8 million acre [6.8 million hectare]) national forest wilderness means undisturbed fish and wildlife habitat, (U.S. Forest Service [USFS] 2003). which in turn translates into food, employment, and The Wilderness Act of 1964 provides a legal business. These wilderness values are realized in definition for wilderness. As an indicator of wild subsistence, sport and commercial fisheries, and many character, the act has ensured the preservation of facets of tourism and outdoor recreation. To Americans federal lands displaying wilderness qualities important more broadly, wilderness takes on a less utilitarian to recreation, science, ecosystem integrity, spiritual value and is often described in terms of its aesthetic or values, opportunities for solitude, and wildlife needs. spiritual significance. Section 2(c) of the Wilderness Act captures the essence of wilderness by identifying specific qualities that make it unique. The provisions suggest wilderness is an area or region characterized by the following conditions (USFS 2002): Section 2(c)(1) …generally appears to have been affected primarily by the forces of nature, with the imprint of man’s work substantially unnoticeable; Section 2(c)(2) …has outstanding opportunities for solitude or a primitive and unconfined type of recreation; Section 2(c)(3) …has at least five thousand acres of land or is of sufficient FIG 1.
    [Show full text]
  • Pamphlet to Accompany Scientific Investigations Map 3131
    Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3
    [Show full text]
  • VGP) Version 2/5/2009
    Vessel General Permit (VGP) Version 2/5/2009 United States Environmental Protection Agency (EPA) National Pollutant Discharge Elimination System (NPDES) VESSEL GENERAL PERMIT FOR DISCHARGES INCIDENTAL TO THE NORMAL OPERATION OF VESSELS (VGP) AUTHORIZATION TO DISCHARGE UNDER THE NATIONAL POLLUTANT DISCHARGE ELIMINATION SYSTEM In compliance with the provisions of the Clean Water Act (CWA), as amended (33 U.S.C. 1251 et seq.), any owner or operator of a vessel being operated in a capacity as a means of transportation who: • Is eligible for permit coverage under Part 1.2; • If required by Part 1.5.1, submits a complete and accurate Notice of Intent (NOI) is authorized to discharge in accordance with the requirements of this permit. General effluent limits for all eligible vessels are given in Part 2. Further vessel class or type specific requirements are given in Part 5 for select vessels and apply in addition to any general effluent limits in Part 2. Specific requirements that apply in individual States and Indian Country Lands are found in Part 6. Definitions of permit-specific terms used in this permit are provided in Appendix A. This permit becomes effective on December 19, 2008 for all jurisdictions except Alaska and Hawaii. This permit and the authorization to discharge expire at midnight, December 19, 2013 i Vessel General Permit (VGP) Version 2/5/2009 Signed and issued this 18th day of December, 2008 William K. Honker, Acting Director Robert W. Varney, Water Quality Protection Division, EPA Region Regional Administrator, EPA Region 1 6 Signed and issued this 18th day of December, 2008 Signed and issued this 18th day of December, Barbara A.
    [Show full text]
  • Bulletin of the United States Fish Commission
    SALMON-TAGGING EXPERIMENTS IN ALASKA, 1924 AND 1925 1 .:I- By WILLIS H. RICH, Ph. D. Director, U. S. Biological Station, Seattle, Wash; .:I­ CONTENTS Page Introduction _ 109 Experiments in southeastern Alaska__hhu u __nn_h__u u u _ 116 Tagging record _ 116 Returns from experiments in Icy Strait__ n h_u u_..u u _ 119 Returns from experiments in Frederick Sound u huh _ 123 Returns from experiments in Chatham Strait; h u • _ 123 Returns from experiments in Sumner Strait, u_uuu .. u _ 128 Returns from experiments at Cape Muzon and Kaigani Point, ~ _ 135 Returns from experiments at Cape Chacon u n u h _ 137 Returns from experiments near Cape Fox and Duke Islandu _ 141 Variations in returns of tagged fish; h _u u n n h n __ h u_ 143 Conelusions _ 144 Experiments at Port Moller, 1925un__h_uu uu __ 145 INTRODUCTION The extensive salmon-tagging experiments conducted during 1922 and 1923 2 in the region of the Alaska Peninsula proved so productive of information, both of scientific interest and of practical application in the care of these fisheries, that it was considered desirable to undertake similar investigations in other districts; Accordingly, experiments were carried on in southeastern Alaska in 1924 and again in 1925. In 1925, also, at the request of one of the companies engaged in packing salmon in the Port Moller district, along the northern shore of the Alaska Penin­ sula, the work done there in 1922 was repeated. The results of these experiments form the basis for the following report.
    [Show full text]
  • APPLICATIONS of QUANTITATIVE METHODS and CHAOS THEORY in ICHNOLOGY for ANALYSIS of INVERTEBRATE BEHAVIOR and EVOLUTION by James
    APPLICATIONS OF QUANTITATIVE METHODS AND CHAOS THEORY IN ICHNOLOGY FOR ANALYSIS OF INVERTEBRATE BEHAVIOR AND EVOLUTION by James Richard Woodson Lehane A dissertation submitted to the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Department of Geology and Geophysics The University of Utah August 2014 Copyright © James Richard Woodson Lehane 2014 All Rights Reserved The University of Utah Graduate School STATEMENT OF DISSERTATION APPROVAL The dissertation of James Richard Woodson Lehane has been approved by the following supervisory committee members: Allan A. Ekdale , Chair May 5th, 2014 Date Approved Randall B. Irmis , Member June 6th, 2014 Date Approved Marjorie A. Chan , Member May 5th, 2014 Date Approved Elena A. Cherkaev , Member June 12th, 2014 Date Approved Leif Tapanila , Member June 6th, 2014 Date Approved and by John M. Bartley , Chair/Dean of the Department/College/School of Geology and Geophysics and by David B. Kieda, Dean of The Graduate School. ABSTRACT Trace fossils are the result of animal behaviors, such as burrowing and feeding, recorded in the rock record. Previous research has been mainly on the systematic description of trace fossils and their paleoenvironmental implications, not how animal behaviors have evolved. This study analyzes behavioral evolution using the quantification of a group of trace fossils, termed graphoglyptids. Graphoglyptids are deep marine trace fossils, typically found preserved as casts on the bottom of turbidite beds. The analytical techniques performed on the graphoglyptids include calculating fractal dimension, branching angles, and tortuosity, among other analyses, for each individual trace fossil and were performed on over 400 trace fossils, ranging from the Cambrian to the modem.
    [Show full text]
  • Fossil Mosses: What Do They Tell Us About Moss Evolution?
    Bry. Div. Evo. 043 (1): 072–097 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.7 Fossil mosses: What do they tell us about moss evolution? MicHAEL S. IGNATOV1,2 & ELENA V. MASLOVA3 1 Tsitsin Main Botanical Garden of the Russian Academy of Sciences, Moscow, Russia 2 Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia 3 Belgorod State University, Pobedy Square, 85, Belgorod, 308015 Russia �[email protected], https://orcid.org/0000-0003-1520-042X * author for correspondence: �[email protected], https://orcid.org/0000-0001-6096-6315 Abstract The moss fossil records from the Paleozoic age to the Eocene epoch are reviewed and their putative relationships to extant moss groups discussed. The incomplete preservation and lack of key characters that could define the position of an ancient moss in modern classification remain the problem. Carboniferous records are still impossible to refer to any of the modern moss taxa. Numerous Permian protosphagnalean mosses possess traits that are absent in any extant group and they are therefore treated here as an extinct lineage, whose descendants, if any remain, cannot be recognized among contemporary taxa. Non-protosphagnalean Permian mosses were also fairly diverse, representing morphotypes comparable with Dicranidae and acrocarpous Bryidae, although unequivocal representatives of these subclasses are known only since Cretaceous and Jurassic. Even though Sphagnales is one of two oldest lineages separated from the main trunk of moss phylogenetic tree, it appears in fossil state regularly only since Late Cretaceous, ca.
    [Show full text]
  • Division 300 Bases Section 304 Aggregate Base Course Description
    304.07 DIVISION 300 BASES SECTION 304 AGGREGATE BASE COURSE DESCRIPTION 304.01 This work consists of furnishing and placing one or more courses of aggregate and additives, if required, on a prepared subgrade. MATERIALS 304.02 Aggregate. The aggregates shall meet the requirements of subsection 703.03. Acceptance will be based on random samples taken from each lift. 304.03 Commercial Mineral Fillers. Portland cement shall conform to subsection 701.01. Hydrated lime shall conform to subsection 712.03. CONSTRUCTION REQUIREMENTS 304.04 Placing. If the required compacted depth of the aggregate base course exceeds 6 inches, it shall be constructed in two or more layers of approximately equal thickness. The maximum compacted thickness of any one layer shall not exceed 6 inches. When vibratory or other approved types of special compacting equipment are used, the compacted depth of a single layer may be increased to 8 inches upon request, provided that specified density is achieved and written approval is given. 304.05 Mixing. The Contractor shall mix the aggregate by methods that insure a thorough and homogenous mixture. 304.06 Shaping and Compaction. Compaction of each layer shall continue until a density of at least 95 percent of the maximum density has been achieved as determined in accordance with AASHTO T 180 as modified by CP 23. The moisture content shall be at ± 2 percent of optimum moisture content. The surface of each layer shall be maintained during the compaction operations so that a uniform texture is produced and the aggregates are firmly keyed. Moisture conditioning shall be performed uniformly during compaction.
    [Show full text]
  • Full-Text PDF (Final Published Version)
    Pritchard, M. E., de Silva, S. L., Michelfelder, G., Zandt, G., McNutt, S. R., Gottsmann, J., West, M. E., Blundy, J., Christensen, D. H., Finnegan, N. J., Minaya, E., Sparks, R. S. J., Sunagua, M., Unsworth, M. J., Alvizuri, C., Comeau, M. J., del Potro, R., Díaz, D., Diez, M., ... Ward, K. M. (2018). Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes. Geosphere, 14(3), 954-982. https://doi.org/10.1130/GES01578.1 Publisher's PDF, also known as Version of record License (if available): CC BY-NC Link to published version (if available): 10.1130/GES01578.1 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Geo Science World at https://doi.org/10.1130/GES01578.1 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes GEOSPHERE; v. 14, no. 3 M.E. Pritchard1,2, S.L. de Silva3, G. Michelfelder4, G. Zandt5, S.R. McNutt6, J. Gottsmann2, M.E. West7, J. Blundy2, D.H.
    [Show full text]
  • Thermochronology of the Talkeetna Intraoceanic Arc of Alaska: Ar/Ar, U‐Th/He, Sm‐Nd, and Lu‐Hf Dating
    TECTONICS, VOL. 30, TC1011, doi:10.1029/2010TC002798, 2011 Thermochronology of the Talkeetna intraoceanic arc of Alaska: Ar/Ar, U‐Th/He, Sm‐Nd, and Lu‐Hf dating B. R. Hacker,1 Peter B. Kelemen,2 Matthew Rioux,1,3 Michael O. McWilliams,4 Philip B. Gans,1 Peter W. Reiners,5 Paul W. Layer,6 Ulf Söderlund,7 and Jeffrey D. Vervoort8 Received 17 September 2010; revised 8 December 2010; accepted 27 December 2010; published 26 February 2011. [1] As one of two well‐exposed intraoceanic arcs, the of the Talkeetna arc was spatially variable. One‐ Talkeetna arc of Alaska affords an opportunity to under- dimensional finite difference thermal models show that stand processes deep within arcs. This study reports new this kind of spatial variability is inherent to intraoceanic Lu‐Hf and Sm‐Nd garnet ages, 40Ar/39Ar hornblende, arcs with simple construction histories. Citation: Hacker, mica and whole‐rock ages, and U‐Th/He zircon and B. R., P. B. Kelemen, M. Rioux, M. O. McWilliams, P. B. Gans, apatite ages from the Chugach Mountains, Talkeetna P. W. Reiners, P. W. Layer, U. Söderlund, and J. D. Vervoort Mountains, and Alaska Peninsula, which, in conjunc- (2011), Thermochronology of the Talkeetna intraoceanic arc of tion with existing geochronology, constrain the thermal Alaska: Ar/Ar, U‐Th/He, Sm‐Nd, and Lu‐Hf dating, Tectonics, history of the arc. Zircon U‐Pb ages establish the 30, TC1011, doi:10.1029/2010TC002798. main period of arc magmatism as 202–181 Ma in the Chugach Mountains and 183–153 Ma in the 1.
    [Show full text]