Ble of Information Contained in DOE's Research and Development Reports to Business, Industry, the Academic Community, and Federal, State and Local Governments

Total Page:16

File Type:pdf, Size:1020Kb

Ble of Information Contained in DOE's Research and Development Reports to Business, Industry, the Academic Community, and Federal, State and Local Governments A major purpose of the Techni- cal Information Center is to provide / the broadest dissemination possi- ble of information contained in DOE's Research and Development Reports to business, industry, the academic community, and federal, state and local governments. Although a small portion of this report is not reproducible, it is being made available to expedite the availability of information on the research discussed herein. ORNL/Sub—84-64794/1 )DE8.5 010453 SHALES AND OTHER ARGILLACEOUS STRATA IN THE UNITED STATES *3erge Gonzales Earth Resource Associates, Inc. Athens, Georgia 30601 Kenneth S. Johnson University of Oklahoma P i Norman, Oklahoma 73069 s. q. r SI- BT3 <S g5 WHfs-g 5' g s -3 n. sn? f ffP g S- 5" — > a ii 8 3 a 3 I g- Date Published: March 1985 1 - — G2 3 ^ S 5 2 3 - J! sg o=r a. 3a ^I» t» I © 3 3. 55 8 ^ n A ••55 Report Prepared by 5FF a. 8B bG c <8 Earth Resources Associates, Inc. Q o _ 3. 2 o Athens, Georgia hmr=> 3 5 8 I ; under 3 E- « i P9 Subcontract No. 11X-64794V S^l 8 1- for ^ u fi* i o g ft- ~ 2. J S g to Ef >< Oak Ridge National Laboratory _ vN; o BSO. o 1I Oak Ridge, Tennessee 37831 operated by if»s s s MARTIN MARIETTA ENERGY SYSTEMS, INC. lllil for the Mftl U.S. DEPARTMENT OF ENERGY under Contract No. DE-AC05-840R21400 s1 I is-?: \ DISTRIBUTION CF T11IS DOCUMENT IS UUUMITta iii FOREWORD In 1976 the National Waste Terminal Storage (NWTS) Program was established by the U.S. Energy Research and Development Administration (ERDA), the agency that has now become the U.S. Department of Energy (DOE). The NWTS Program is directed toward development of technology for the permanent disposal of high-level radioactive waste in an environmentally safe manner. Emphasis has been placed on disposal of the wastes deep underground in repositories constructed in geologically stable rocks. Several rock types are being considered by the DOE as host rocks for disposal of wastes; these rocks include basalt, crystalline rock (granitic), volcanic tuff, salt, and various other sedimentary rocks, such as shales and argillaceous strata. In 1979, the DOE, through the Office of Nuclear Waste Isolation (ONWI) at Battelle Memorial Institute, contracted with Serge Gonzales and Kenneth S. Johnson to prepare a report on the geologic and hydrologic characterization of shales and other argillaceous strata in the conterminous United States. This report was to serve as a data base for further assessment of such rocks as possible candidates for hosting a repository. The report was first produced by ONWI in preliminary draft form in 1982. In 1984, the DOE requested that Oak Ridge National Laboratory (ORNL) issue this second, revised draft of the report for review, as part of ORNL's program to investigate sedimentary rocks other than salt for waste disposal purposes. With one exception, revisions made in preparing the second draft have not incorporated geologic data and reports issued since the first draft was prepared, and, thus, the effective date for information upon which this revised draft is based is early 1982. Because of new geologic data, developed by ORNL staff, on the Conasauga Group of rocks, the description of this group has been updated to include publications since 1982. This report presents detailed geologic and hydrologic data that describe shales and other argillaceous rocks; data are from the open literature. These data are intended to be used in the future to aid in assessment of various strata and their potential for repository siting. No observations, conclusions, or recommendations are made by the authors of this report relative to the suitability of various argillaceous rocks for waste disposal. There are, however, other published reports that contain technical data and evaluative statements regarding the suitability of various argillaceous rocks for repository siting. Where appropriate, the authors of this report have referenced this previously published literature and have summarized the technical data. The authors acknowledge the cooperation and support provided by staff members of ONWI, Battelle Memorial Institute, especially R. B. Laughon, who provided guidance in preparation and review of the first draft of this report. The authors also wish to thank S. H. Stow, ORNL, for his support and review of the first draft and his supervision during preparation of the second draft; C. S. Haase, ORNL, for his aid in updating the section on the Conasauga Group; J. Ingram for drafting the illustrations; and N. G. Allred for preparing the final typed copy of the report. V TABLE OF CONTENTS Page 1. INTRODUCTION 1 1.1 BACKGROUND 1 1.2 GEOLOGIC PROPERTIES OF SHALE 4 1.2.1 Terminology 5 1.2.2 Mineralogy 7 1.2.3 Diagenesis 10 1.3 REGIONAL GEOLOGIC CHARACTERISTICS IMPORTANT FOR WASTE DISPOSAL 12 1.3.1 Structure and Geologic Framework 12 1.3.2 Shale Deposits As Repository Host Rocks 14 1.3.3 Seismic Activity 15 1.3.4 Hydrology 16 1.3.5 Mineral Resources 20 2. PRINCIPAL SHALES IN THE UNITED STATES 21 2.1 DEPOSITION OF SHALES '.. 21 2.2 DISTRIBUTION OF PRINCIPAL SHALES 22 3. EASTERN INTERIOR 27 3.1 STRUCTURE AND GEOLOGIC FRAMEWORK .. 27 3.2 REGIONAL SEISMICITY 40 3.3 REGIONAL HYDROLOGY 41 3.3.1 Surface Water 41 3.3.2 Ground Water 44 3.4 SHALES AND ARGILLACEOUS STRATA 49 3.4.1 Introduction 49 3.4.2 Maquoketa Group 50 3.4.3 Cincinnatian Series 62 3.4.4 Devonian-Mississippian Shales 73 3.4.5 Other Units Ill 3.5 REG IONAL SUMMARY 116 vi TABLE OF CONTENTS (Continued) Pa8e 4. EASTERN MARGIN . 119 4.1 STRUCTURE AND GEOLOGIC FRAMEWORK 119 4.2 REGIONAL SEISMICITY 126 4.3 REGIONAL HYDROLOGY 130 4.3.1 Surface Water 130 4.3.2 Ground Water 132 4.4 SHALES AND ARGILLACEOUS UNITS 137 4.4.1 Introduction % 137 4.4.2 Triassic Basic Shales 137 4.4.3 Other Units 142 4.5 REGIONAL SUMMARY 154 5. GULF COAST 157 5.1 STRUCTURE AND GEOLOGIC FRAMEWORK 157 5.2 REGIONAL SEISMICITY 160 5.3 REGIONAL HYDROLOGY 161 5.3.1 Surface Water 161 5.3.2 Ground Water 162 5.4 SHALES AND ARGILLACEOUS UNITS 164 5.4.1 Introduction 164 5.4.2 Porters Creek Clay 165 5.4.3 Cane River Formation 176 5.4.4 Cook Mountain Formation 183 5.4.5 Yazoo Clay 185 5.4.6 Other Units 192 5.5 REGIONAL SUMMARY 195 6. GREAT PLAINS 197 6.1 STRUCTURE AND GEOLOGIC FRAMEWORK 197 6.2 REGIONAL SEISMICITY 200 vii TABLE OF CONTENTS (Continued) Page 6.3 REGIONAL HYDROLOGY 201 6.3.1 Surface Water 201 6.3.2 Ground Water 202 6.4 SHALES AND ARGILLACEOUS UNITS 204 6.4.1 Introduction 204 6.4.2 Woe:?ford (Chattanooga) Shale 205 6.4.3 Upper Mississippian Shales 220 6.4.4 Pennsylvanian Shales 226 6.4.5 Permian Shales 264 6.4.6 Pierre Shale and Equivalent Upper Cretaceous Shales 276 6.4.7 Lower Cretaceous Shales 298 6.4.8 Colorado Shale and Equivalent Upper Cretaceous Shales 304 6.4.9 Other Units 309 6.5 REGIONAL SUMMARY 311 7. ROCKY MOUNTAINS 317 7.1 STRUCTURE AND GEOLOGIC FRAMEWORK 317 7.2 REGIONAL SEISMICITY 320 7.3 REGIONAL HYDROLOGY 321 7.3.1 Surface Water 321 7.3.2 Ground Water 322 7.4 SHALES AND ARGILLACEOUS UNITS 323 7.4.1 Introduction 323 7.4.2 Milligen Formation and Cooper Basin Group 323 7.4.3 Mowry Shale and Other Lower Cretaceous Shales... 330 7.4.4 Cody Shale and Other Upper Cretaceous Shales.... 338 7.4.5 Tertiary Shales 343 7.4.6 Other Units 351 7.5 REGIONAL SUMMARY 353 viii TABLE OF CONTENTS (Continued) Page 8. COLORADO PLATEAU 355 8.1 STRUCTURE AND GEOLOGIC FRAMEWORK 355 8.2 REGIONAL SEISMICITY 357 8.3 REGIONAL HYDROLOGY 357 8.3.1 Surface Water 357 8.3.2 Ground Water 358 8.4 SHALES AND ARGILLACEOUS UNITS 359 8.4.1 Introduction 359 8.4.2 Mancos Shale and Other Upper Cretaceous Shales.. 360 8.4.3 Green River Formation 375 8.4.4 Other Units • 384 8.5 REGIONAL SUMMARY 387 9. GREAT BASIN OF NEVADA AND UTAH 391 9.1 STRUCTURE AND GEOLOGIC FRAMEWORK 391 9.2 REGIONAL SEISMICITY 395 9.3 REGIONAL HYDROLOGY 395 9.3.1 Surface Water 395 9.3.2 Ground Water 396 9.4 SHALES AND ARGILLACEOUS UNITS 397 9.4.1 Introduction 397 9.4.2 Eleana Formation..... 398 9.4.3 Pilot Shale and Chainman Shale 409 9.4.4 Other Units 414 9.5 REGIONAL SUMMARY 416 10. GREAT VALLEY OF CALIFORNIA 417 10.1 STRUCTURE AND GEOLOGIC FRAMEWORK 417 10.2 REGIONAL SEISMICITY 420 ix TABLE OF CONTENTS (Continued) Page 10.3 REGIONAL HYDROLOGY 421 10.3.1 Surface Water 421 10.3.2 Ground Water 423 10.4 SHALES AND ARGILLACEOUS UNITS 424 10.4.1 Introdution 424 10.4.2 Stratigraphy 425 i 10.4.3 Geologic Setting 433 10.4.4 Mineralogy and Rock Properties 436 10.4.5 Hydrology 438 10.4.6 Mineral Resources 439 10.5 REGIONAL SUMMARY 442 11. PACIFIC NORTHWEST 445 11.1 STRUCTURE AND GEOLOGIC FRAMEWORK 445 11.2 REGIONAL SEISMICITY 448 11.3 REGIONAL HYDROLOGY „ 449 11.3.1 Surface Water 449 . 11.3.2 Ground Water 450 11.4 SHALES AND ARGILLACEOUS UNITS 451 11.4.1 Introduction 451 11.4.2 Bastendorff Formation 451 11.4.3 Toledo Formation and Nye Mudstone 455 11.4.4 Twin River Formation 459 11.5 REGIONAL SUMMARY 463 ! 12.
Recommended publications
  • Hydrogeologic Framework of Mississippian Rocks in the Central Lower Peninsula of Michigan
    Hydrogeologic Framework of Mississippian Rocks in the Central Lower Peninsula of Michigan By D.B. WESTJOHN and T.L. WEAVER U.S. Geological Survey Water-Resources Investigations Report 94-4246 Lansing, Michigan 1996 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director Any use of trade, product, or firm name in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. For additional information Copies of this report may be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey, WRD Earth Science Information Center 6520 Mercantile Way, Suite 5 Open-File Reports Section Lansing, Ml 48911 Box 25286, MS 517 Denver Federal Center Denver, CO 80225 CONTENTS Abstract .......................................................... 1 Introduction ....................................................... 1 Geology .......................................................... 3 Coldwater Shale ................................................ 3 Marshall Sandstone .............................................. 6 Michigan Formation .............................................. 7 Hydrogeologic framework of Mississippian rocks ................................ 8 Relations of stratigraphic units to aquifer and confining units .................... 8 Delineation of aquifer- and confining-unit boundaries ......................... 9 Description of confining units and the Marshall aquifer ........................ 9 Michigan confining
    [Show full text]
  • Stratographic Coloumn of Iowa
    Iowa Stratographic Column November 4, 2013 QUATERNARY Holocene Series DeForest Formation Camp Creek Member Roberts Creek Member Turton Submember Mullenix Submember Gunder Formation Hatcher Submember Watkins Submember Corrington Formation Flack Formation Woden Formation West Okoboji Formation Pleistocene Series Wisconsinan Episode Peoria Formation Silt Facies Sand Facies Dows Formation Pilot Knob Member Lake Mills Member Morgan Member Alden Member Noah Creek Formation Sheldon Creek Formation Roxana/Pisgah Formation Illinoian Episode Loveland Formation Glasford Formation Kellerville Memeber Pre-Illinoian Wolf Creek Formation Hickory Hills Member Aurora Memeber Winthrop Memeber Alburnett Formation A glacial tills Lava Creek B Volcanic Ash B glacial tills Mesa Falls Volcanic Ash Huckleberry Ridge Volcanic Ash C glacial tills TERTIARY Salt & Pepper sands CRETACEOUS "Manson" Group "upper Colorado" Group Niobrara Formation Fort Benton ("lower Colorado ") Group Carlile Shale Greenhorn Limestone Graneros Shale Dakota Formation Woodbury Member Nishnabotna Member Windrow Formation Ostrander Member Iron Hill Member JURASSIC Fort Dodge Formation PENNSYLVANIAN (subsystem of Carboniferous System) Wabaunsee Group Wood Siding Formation Root Formation French Creek Shale Jim Creek Limestone Friedrich Shale Stotler Formation Grandhaven Limestone Dry Shale Dover Limestone Pillsbury Formation Nyman Coal Zeandale Formation Maple Hill Limestone Wamego Shale Tarkio Limestone Willard Shale Emporia Formation Elmont Limestone Harveyville Shale Reading Limestone Auburn
    [Show full text]
  • PROFESSIONAL PAPER 1418 USGS Cience for a Changing World AVAILABILITY of BOOKS and MAPS of the U.S
    PROFESSIONAL PAPER 1418 USGS cience for a changing world AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current- year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publica­ tions released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may be no longer available. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech­ Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey Earth of general interest (such as leaflets, pamphlets, booklets), single Science Information Centers (ESIC's), all of which are authorized copies of Preliminary Determination of Epicenters, and some mis­ agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are ANCHORAGE, Alaska Rm. 101,4230 University Dr. obtainable by mail from LAKEWOOD, Colorado Federal Center, Bldg. 810 U.S. Geological Survey, Information Services MENLO PARK, California Bldg. 3, Rm.
    [Show full text]
  • Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois
    2UJ?. *& "1 479 S 14.GS: CIR479 STATE OF ILLINOIS c. 1 DEPARTMENT OF REGISTRATION AND EDUCATION Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois H. B. Willman GEOLOGICAL ILLINOIS ""SURVEY * 10RM* APR 3H986 ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief Urbano, IL 61801 CIRCULAR 479 1973 CONTENTS Page Abstract 1 Introduction 1 Time-stratigraphic classification 3 Alexandrian Series 5 Niagaran Series 5 Cayugan Series 6 Regional correlations 6 Northeastern Illinois 6 Development of the classification 9 Wilhelmi Formation 12 Schweizer Member 13 Birds Member 13 Elwood Formation 14 Kankakee Formation 15 Drummond Member 17 Offerman Member 17 Troutman Member 18 Plaines Member 18 Joliet Formation 19 Brandon Bridge Member 20 Markgraf Member 21 Romeo Member 22 Sugar Run Formation . „ 22 Racine Formation 24 Northwestern Illinois 26 Development of the classification 29 Mosalem Formation 31 Tete des Morts Formation 33 Blanding Formation 35 Sweeney Formation 36 Marcus Formation 3 7 Racine Formation 39 References 40 GEOLOGIC SECTIONS Northeastern Illinois 45 Northwestern Illinois 52 FIGURES Figure 1 - Distribution of Silurian rocks in Illinois 2 2 - Classification of Silurian rocks in northeastern and northwestern Illinois 4 3 - Correlation of the Silurian formations in Illinois and adjacent states 7 - CM 4 Distribution of Silurian rocks in northeastern Illinois (modified from State Geologic Map) 8 - lis. 5 Silurian strata in northeastern Illinois 10 ^- 6 - Development of the classification of the Silurian System in |§ northeastern Illinois 11 7 - Distribution of Silurian rocks in northwestern Illinois (modified ;0 from State Geologic Map) 2 7 8 - Silurian strata in northwestern Illinois 28 o 9 - Development of the classification of the Silurian System in CO northwestern Illinois 30 10 - Index to stratigraphic units described in the geologic sections • • 46 ROCK STRATIGRAPHY OF THE SILURIAN SYSTEM IN NORTHEASTERN AND NORTHWESTERN ILLINOIS H.
    [Show full text]
  • Download File
    Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming.
    [Show full text]
  • Stratigraphic Succession in Lower Peninsula of Michigan
    STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation
    [Show full text]
  • Guide to the Geology of Northeastern Ohio
    SDMS US EPA REGION V -1 SOME IMAGES WITHIN THIS DOCUMENT MAY BE ILLEGIBLE DUE TO BAD SOURCE DOCUMENTS. GUIDE TO THE GEOLOGY of NORTHEASTERN OHIO Edited by P. O. BANKS & RODNEY M. FELDMANN 1970 Northern Ohio Geological Society ELYP.i.A PU&UC LIBRARt as, BEDROCK GEOLOGY OF NORTHEASTERN OHIO PENNSYLVANIAN SYSTEM MISSISSIPPIAN SYSTEM DEVONIAN SYSTEM \V&fe'£:i£:VS:#: CANTON viSlSWSSWM FIGURr I Geologic map of northeastern Ohio. Individual formations within each time unit are not dis- -guished, and glacial deposits have been omitted. Because the bedding planes are nearly ••.crizontal, the map patterns of the contacts closely resemble the topographic contours at those z evations. The older and deeper units are most extensively exposed where the major rivers rave cut into them, while the younger units are preserved in the intervening higher areas. CO «< in Dev. Mississippian r-c Penn. a> 3 CO CD BRADF. KINOERHOOK MERAMEC —1 OSAGE CHESTER POTTSVIUE ro to r-» c-> e-> e= e-i GO n « -n V) CO V* o ^_ ^ 0. = -^ eo CO 3 c= « ^> <C3 at ta B> ^ °» eu ra to a O9 eo ^ a* s 1= ca \ *** CO ^ CO to CM v» o' CO to CO 3 =3 13- *•» \ ¥\ A. FIGURE 1. Columnar section ol the major stratigraphic units in northeastern Ohio showing their relative positions in the standard geologic time scale. The Devonian-Mississippian boundary is not known with certainty to lie within the Cleveland Shale. The base of the Mississippian in the northern part of the state is transitional with the Bradford Series of the Devonian System and may lie within the Cleveland Shale (Weller er a/., 1948).
    [Show full text]
  • Deep Oil Possibilities of the Illinois Basin
    s Ccc 36? STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell Elwood Atherton T. C. Buschbach David H. Swann ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 368 1964 . DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell, Elwood Atherton, T. C. Buschbach, and David H. Swann ABSTRACT The Middle Ordovician and younger rocks of the Illinois Basin, which have yielded 3 billion barrels of oil, are underlain by a larger volume of virtually untested Lower Ordovician and Cambrian rocks. Within the region that has supplied 99 percent of the oil, where the top of the Middle Ordovician (Trenton) is more than 1,000 feet be- low sea level, less than 8 inches of hole have been drilled per cubic mile of the older rocks. Even this drilling has been near the edges; and in the central area, which has yielded five- sixths of the oil, only one inch of test hole has been drilled per cubic mile of Lower Ordovician and Cambrian. Yet drilling depths are not excessive, ranging from 6,000 to 14,000 feet to the Precambrian. More production may be found in the Middle Ordovician Galena Limestone (Trenton), thus extending the present productive regions. In addition, new production may be found in narrow, dolomitized fracture zones in the tight limestone facies on the north flank of the basin . The underlying Platteville Limestone is finer grained and offers fewer possibilities. The Joachim Dolomite oil- shows occur in tight sandstone bodies that should have commercial porosity in some re- gions.
    [Show full text]
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • VDRARY FEB / Marine Science Laboratory Oregon State University
    0) VDRARY FEB / Marine Science Laboratory Oregon State University Vol. 37, No. 1 January 1975 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES The Ore Bin Published Monthly By sr* STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Portland, Oregon - 97201 Telephone: [503] - 229-5580 FIELD OFFICES 2033 First Street 521 N. E. "E" Street Baker 97814 Grants Pass 97526 XX X XX X X XXX X XXX X XXX X X Subscription Rate 1 year - $2.00; 3 years - $5.00 Available back issues - $.25 each Second class postage paid at Portland, Oregon 9 9 9 9 9 9 9 9 9 5Z 9 9' 9 9 9 9 9 9 9 '9 0. GOVERNING BOARD R. W. deWeese, Portland, Chairman William E. Miller, Bend H. Lyle Van Gordon, Grants Pass STATE GEOLOGIST R. E. Corcoran GEOLOGISTS IN CHARGE OF FIELD OFFICES Howard C. Brooks, Baker Len Ramp, Grants Pass 5Z 9 5Z 9 9 9' 5Z 5Z 5Z 5Z 5Z 9' 9 5Z x 5Z 5Z 'k 5Z 5Z Permission is granted to reprint information contained herein. Credit given the State of Oregon Department of Geology and Mineral Industries • for compiling this information will be appreciated. State of Oregon The ORE BIN Department of Geology Volume 37,No. 1 and Mineral Industries January 1975 • 069 State Office Bldg. rtland Oregon 97201 OREGON'S MINERAL AND METALLURGICAL INDUSTRY IN 1974 Ralph S. Mason, Deputy State Geologist Oregon Department of Geology and Mineral Industries The value of raw minerals produced in the State during 1974 increased 11.3 percent, eclipsing a gain of nearly 9 percent for the previous year.
    [Show full text]
  • Tonto Creek Total Nitrogen TMDL Effectiveness Monitoring Report Recommendation for Delisting
    Tonto Creek Total Nitrogen TMDL Effectiveness Monitoring Report Recommendation for Delisting Executive Summary Tonto Creek was placed on Arizona’s Water Quality Impaired Waters List 303(d) for Total Nitrogen initially in 1996 due to exceeding the aquatic and wildlife cold water (A&Wc) and warm water (A&Ww) designated uses. Total Nitrogen on Tonto Creek has an annual mean standard of 0.5 milligrams per liter (mg/L) and a single sample maximum (SSM) standard of 2.0 mg/L. Two reaches of Tonto Creek were listed as impaired due to exceedances of the annual mean nitrogen standard, Reach 013A is the headwaters to confluence with unnamed tributary at N 34° 18’ 10”/W 111° 04’ 14” and Reach 013B is Tonto Creek from unnamed tributary at N 34° 18’ 10”/W 111° 04’ 14” to Haigler Creek. The Total Nitrogen Total Maximum Daily Load (TMDL) was completed in June 2005. The TMDL identified several nonpoint sources as contributors to Total Nitrogen concentrations in Tonto Creek including recreational uses and unincorporated communities/summer home clusters (ADEQ 2005). There is also a permitted point source in the watershed, Arizona Game and Fish Department’s (AGFD) Tonto Creek Fish Hatchery. The 2005 Tonto Creek TMDL recommended implementation projects and appropriate best management practices (BMPs) to decrease the Total Nitrogen levels in Tonto Creek. Through Arizona Department of Environmental Quality (ADEQ) Water Quality Improvement Grant (WQIG) funding and other projects, septic system upgrades were made throughout the impaired watershed. AGFD also made several upgrades to the facility. These projects working in concert with each other were effective in reducing Total Nitrogen loads in Tonto Creek.
    [Show full text]
  • Uppermost Cretaceous and Tertiary Stratigraphy of Fossil Basin, Southwestern Wyoming
    Uppermost Cretaceous and Tertiary Stratigraphy of Fossil Basin, Southwestern Wyoming By STEVEN S. ORIEL and JOSHUA I. TRACEY, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 635 New subdivisions of the J,ooo-Joot-thick continental Evanston, Wasatch, Green River, and Fowkes Formations facilitate understanding of sediment genesis and Jl7yoming thrust-belt tectonic events UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-604646 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 65 cents (paper cover) CONTENTS Page Wasatch Formation-Continued Abstract __________________________________________ _ 1 Fossils and age-Continued· Page Introduction ______________________________________ _ 2 Tunp Member______________________________ 28 Purpose ______________________________________ _ 2 Origin--------~-------------------------------- 28 Earlier work_ .. __ - __ - ___________________ - _-- _- __ 2 Tectonic implications ____________ -_-------------- 29 Acknowledgments __ . ___________________________ _ 2 Green River Formation ___ .. _______ ------------------ 30 General relations ___ -- _________________________ _ 5 Name and usage __________________ -------------- 30 Evanston Formation _______________________________ _ 5 Definition __________________ -_-------------- 30 N arne and usage _______________________________ _ 5 Lithologic heterogeneity.
    [Show full text]