Phosphate in Utah and an Analysis of the Stratigraphy of the Park City And

Total Page:16

File Type:pdf, Size:1020Kb

Phosphate in Utah and an Analysis of the Stratigraphy of the Park City And UTAH GEOLOGICAL AND MINERALOGICAL SURVEY Tho Ut ah Goological and Mineralo,gical SU)'\'ey was authorized by act of the Utah State Le,l';islature in 19:i1; hOWe\'el', no funds were made a\'ailable for its establishmE'nt until 1941 when the State Government was reorganized and the Utah Geological and Mineralogical Sur\'C'y was placeri within the new State Department of Publicity and Industrial De\'E~lopment where the SUf\'ey functioned until .Jul~ 1. 1949, EffectiH' as of that riate, the Survey was tram;­ fern>ri hy law to the ColJe,~e of Mines and Mineral Industries, Uni\'ersity of Utah. The Ut((h Coile A'III/ot((tcri 191,:], Vol. :'!) Title ,q, as an1C'nried by cl/((pte,. ~() LaIC.'; of Utuh 191,9 , pro\'ides that the Utah Geological and Mineralogical SUl'\'ey "shall ha\'(' fo)' its objects": 1. "The co lloction and distribution of rolial>le information regarding the mineral resoul'C('S of tho Sta to, L. "The sUITey of the .l';oo lo,gical formations of the State with special ref­ erence to their economic contents, \'alues and uses, such as: tho oros of the \'Cll'ious metals, coa l. oil-shale, hyrll'o-cal'bons, oil, gas, industrial clays, cement materials, mineral watC'l'S and other surface and underground water supplies. mineral fel'tilizC')'s, asphalt. bitumen, structural materials, road-making ma­ terials, their kind anrl a\'ailability; and the promotion of the markoting of the mineral products of the State. 3. "The inH'stigation of the kind, amount, anri a\ ' ailabilit~ of the \arious mineral substances containod in Stato lands, \\'ith a view of the most efTecti\(.' and profitable arlministration of such lands for the State. 4. "The considNa t ion or such ot her scientific and economic pl'obl('ms as, in the judgment of the Board of l(egents, shoulri come within the field of the SUr\·o y . 5. "Cooperation \\'ith Utah statl' bureaus clealin.l'; with related subjects, with the United States Gcolo,gical Sun'ey anri \\7ith the United States Bureau of Mines, in their l'L'spectin' funct ions inciuding field im'esl igat ions, and thE' preparation, publication, and riistribution of reports and bulletins embodying t he results of the work of tl1<' Survey. 6. "The preparation, publication, distribution and sale of maps. reports and bulletins embodying the ]'(.'sults of thl' work of the Suney. The collection and (,stablishment of exhibits of t he mineral resources of Ut ah. 7. "Any income from the sale of maps and reports or from gifts or from other sources for the Sur\'('y shall he turneri over to the Statc Treasurer and credited hy him to a fund to he known as the Survey Fund to be used under the dircction of th(' Director of the Survey for puhlication of maps, bulletins or other reports of im'estigation of the Geological and Mineralogical Suney." The Utah Geological and Mineralogical Survey has published maps, cir­ culars, and bulletins as well as articles in popular and scientific ma,gazines. For a partial list of these, see the closing pages of this publication. For other informa tion concerning the geological and mineralogical resources of Utah address: ARTHUR L. eRA WFORD, Director UTAH GEOL()(;rC\L AND MINERALOGIC,\L SUf{\'EY College of Mines and Mineral Indust ries University of Utah Salt Lake City, Utah UTAH GEOLOGICAL AND MINERALOGICAL SURVEY AFFILIATED WITH THE COLLEGE OF MINES AND MINERAL INDUSTRIES UNIVERSITY OF UTAH SALT LAKE CITY, UTAH PHOSPHATE IN UTAH And an Analysis of the Stratigraphy of the Park City and the Phosphoria Formations, Utah A Preliminary Report By THOMAS M. CHENEY The Division of Raw Materials of the U. s. Atomic Energy Commission contributed to the financial support of this work. Bulletin 59 July, 1957 Price $1.50 Copyright, University of Utah, 1957 UNIVERSITY OF UTAH A. RAy OLPIN, PH.D., President BOARD OF REGENTS WILLIAM J. O'CONNOR • • • • Chairman SPENCER S. ECCLES • • • Vice-Chairman CLARENCE BAMBERGER. • • • • • • Member ROYDEN G. DERRICK. •• •••• • Member RICHARD L. EVANS • • • • • • • • • • • Member LELAND B. FLINT. • • • • • • • • • • • • Member GEORGE M. FISTER, M.D. ••• • • • • • • • • Member THORPE B. ISAACSON • • • • • • Member J. GRANT IVERSON • • • • • • • President.of Alumni Association 1?x-otncio Member RENDELL N. MABEY. • • Member ORRICE C. MCSHANE. • • • • • • • • • Member MRS. A. U. MINER • • • •• •••• • Member NICHOLAS G. MORGAN, JR.. Member A. RAY OLPIN • • • President of the University of Utah 1?x-otncio Member LAMONT F. TORONTO • • . • . • . Secretary of State 1?x-otncio Member COLLEGE OF MINES AND MINERAL INDUSTRIES ARMAND J. EARDLEY, PH.D., Dean UTAH GEOLOGICAL AND MINERALOGICAL SURVEY ADVISORY BOARD JAMES W. WADE • • • . Chairman CARL J. CHRISTENSEN • · . Member ARMAND J. EARDLEY Member CLAUDE P. HEINER • • • Member MILES P. ROMNEY • • • Member HERBERT A. WAITE • • · • Member J. STEWART WILLIAMS • Member STAFF ARTHUR L. CRAWFORD . • . • . Director DONALD G. PRINCE. • • • Assistant Geologist and Chief Draftsman ELIZABETH V. LARSON Office Manager and Editorial Assistant MARY ANN GREAVES • • • • • Bookkeeper and Curator of the Oil Well Sample Library JOANN DESPAIN • • • Manuscript Typist EMILY J. ROBERTS • • • • • . • Stenographer EVELYN WILSON . • • File and Order Clerk ROSEMARY VAN DYKE • • Assistant Manuscript Typist GERRELD L. PULSIPHER. • • • • • . Draftsman ANDREW E. LATVALA • • • • • • • . Draftsman INGRID M. MATZNER. • • • Draftsman CONTENTS Page LIST OF ILLUSTRATIONS.............................................. 4 FOREWORD ••••••••••••••••••••••• 0 • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • 5 ABS TRAC T •••••••••• ~ •• 0 0 ••••••••••• ' . • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • '7 INTRODUCTION .0 ••• 0 •• 00 ••••••••••••••••••••••••••••••••••••• ·••••••• 9 FJ:ELD WORX ••••••••••••••••••••••••••••••••••••••••••••••••• ·••••••• 9 ACKNOWLEDGMENTSoooo............................................... 10 STRATIGRAPHYUTAH........................................................... OF UPPER PALEOZOIC AIm TRIASSIC ROCIS III NORTHEASTERN 11 STRATIGRAPHY OF THE PHOSPHATIC SHALE MIUmER OF THE DESERET AIm BRAZER. 13 STRATIGRAPHY OF THE PARI CITY AND PHOSPHORIA FORMATIORS............... 15 History of nomenclature........................................ 15 Regional relationships............................................. 17 Park City formation................................................ 19 Lower member of the Park City formation......................... 21 Franson member of the Park City formation....................... 21 Northern Wasatch Mountains................................... 22 Central Wasatch Mountains.................................... 22 Southern Wasatch Mountains •••••••••••••••••••••••• ~.......... 23 Uinta Mountains.............................................. 23 Phosphoria formation............................................... 24 Meade Peak phosphatic shale member of the Phosphoria forma- tion.................................................... 25 Northern Wasatch Mountains~............................. 26 Central Wasatch Mountains............................... 26 ,Southern Wasatch Mountains.............................. 27 Uinta Mountains.......................................... 27 Rex chert member of the Phosphoria formation................ 28 Tosi chert member of the Phosphoria formation............... 28 Kackentire .tongue ot the Woodside formation.................... 29 PHOSPHATE DEPOSITS IN UTAH •••••••••••••••••••••••••••••••••••••••• 31 Mineralogy and petrography..................................... 31 Enrichment of phosphorites by weathering....................... 33 Distribution, grade, and thickness of phosphate deposits....... 35 MissisSippian phosphate deposits............................ 35 Permian phosphate deposits.................................. 40 General relationships.................................... 40 Northern Wasatch Mountains............................... 43 Central Wasatch Mountains................................ 45 Southern Wasatch Mountains............................... 45 Uinta Mountains ••••••••••••••••••••••••••••••· ••• ~ •••••••• 46 CONCLUSIONS ••••••••••••••••••••••••••••••••••••••••••••••••••••••• 48 BIBLIOGRAPHY...................................................... 49 IIDEX ••••••••••••••••••••••••••••••••••••••• ·•••••••••••••••••••••• 53 Guidebooks, bulletins and other publications available through the Utah Geological and Mineralogical Survey......................... 55 -3- LIS T o F ILL U S T RAT ION S Figure Page 1 Index map showing area of this report, localities where sec­ tions were measured and sampled, and the four areal subdivi­ sions discussed in this report............................... 6 2 Columnar sections showing lithology and nomenclature of Upper Paleozoic rocks •••••••••••••••••••••••••••••••••••••••••• ~ •• o 8 '3 Index map showing location and thickness of known occurrences of phosphatic shale of Mississippian age ••••••••••••••••••••• 12 4 Map showing dominant lithology of the rocks of Park City age. 14 5 Diagram showing nomenclature and intertonguing relationships of the Phosphoria and Park City, and Woodside formations be­ tween Phosphoria Gulch, Idaho, and the southern Wasatch Moun- tains, Utah •••••••••••••••••••••••••••••••••••••••••••••••••• 16 6 Diagram showing nomenclature and intertonguing relationships of the Park City, Phosphoria, and Woodside formations between Fort Douglas, Utah, and northwestern Colorado................ 18 7 Map showing the areal variation in lithology................. 20 8 Map showing thickness (in feet) of the
Recommended publications
  • Morrison Formation 37 Cretaceous System 48 Cloverly Formation 48 Sykes Mountain Formation 51 Thermopolis Shale 55 Mowry Shale 56
    THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING By CHRISTOPHER JAY CARSON Bachelor of Science Oklahoma State University 1998 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE July, 2000 THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING Thesis Approved: Thesis Advisor ~~L. ... ~. ----'-"'-....D~e~e:.-g-e----- II ACKNOWLEDGEMENTS I wish to express appreciation to my advisor Dr. Arthur Cleaves for providing me with the opportunity to compile this thesis, and his help carrying out the fieldwork portion of the thesis. My sincere appreciation is extended to my advisory committee members: Dr. Stan Paxton, Dr. Gary Stewart, and Mr. David Schmude. I wish to thank Mr. Schmude especially for the great deal of personal effort he put forth toward the completion of this thesis. His efforts included financial, and time contributions, along with invaluable injections of enthusiasm, advice, and friendship. I extend my most sincere thank you to Dr. Burkhard Pohl, The Big Hom Basin Foundation, and the Wyoming Dinosaur Center. Without whose input and financial support this thesis would not have been possible. In conjunction I would like to thank the staff of the Wyoming Dinosaur Center for the great deal of help that I received during my stay in Thermopolis. Finally I wish to thank my friends and family. To my friends who have pursued this process before me, and with me; thank you very much.
    [Show full text]
  • Montana Bureau of Mines and Geology PRELIMINARY
    Montana Bureau of Mines and Geology PRELIMINARY GEOLOGIC MAP OF PARADISE VALLEY SOUTH-CENTRAL MONTANA by David A. Lopez and Jon C. Reiten Montana Bureau of Mines and Geology Open File Report MBMG 480 2003 This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey under Contract Number: 02HQAG0038. Montana 15 90 Map area 90 15 111° Bozeman Livingston 90 Map area r e 89 v i 45°30' R e n o t s w o l l e Y Emigrant Park Co. Gallatin Co. Pray Chico Miner Corwin Springs Jardine Gardiner YELLOWSTONE NATIONAL PARK 45° MT 3 0 3 6 Miles WY Location of the Paradise Valley map area. 1 CORRELATION OF MAP UNITS Qal Qdf Qrs Qc Qaf Qta Qls Holocene Qat1 Qpg Qgtc Qgoc Qgt Qat2 Qgt8 Qgo8 ? Qat Qat3 Qtr Qat4 QUATERNARY Pleistocene Qat5 Unconformity Qba Unconformity Thr Unconformity Tba Pliocene Tgr Unconformity Ts Miocene Unconformity TERTIARY Thpa Thpb Thpv Td Tdf Tqla Tgcs Tgca Eocene Tslc Tse Unconformity Tft Paleocene Unconformity Kho Kbc Kmi Kcd Unconformity Kls Unconformity Kevt Upper Cretaceous Ke CRETACEOUS Ktc Kco Kcf Kf Km Kmfr Ktf Unconformity Lower Cretaceous Kk Jm Upper Jurassic JURASSIC Je Middle Jurassic JT s R Unconformity TRc Lower Triassic TRIASSIC Unconformity Permi an PERMIAN lPq PMpa PMqa Pennsylvani an PENNSYLVANIAN lPMa Upper Miss. Unconformity MISSISSIPPIAN Mm Lower Miss. Unconformity DOs Dev.—Ord. DEV. --ORD Unconformity U & Mid.Cambrian CAMBRIAN Cs Unconformity Early Proterozoic Xmy PRECAMBRIAN Unconformity Archean Ag Anc Aqa Asg Aga As 2 DESCRIPTIONS OF MAP UNITS Qal Alluvium of modern channels and flood plains (Holocene) – Younger alluvium generally confined to the present flood plain developed along active rivers and streams.
    [Show full text]
  • From the Western of the United
    from the Western of the United GEOLOGICAL SURVEY P R® BES&lON AL PAPER 1057 Early Triassic Terebratulid Brachiopods from the Western Interior of the United States By PETER R. HOOVER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1057 Description and illustration offive species of terebratulid brachiopods, and discussion of their distribution and developmental and evolutionary history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Hoover, Peter R. Early Triassic Terebratulid Brachiopods from the Western Interior of the United States (Geological Survey Professional Paper 1057) Bibliography: p. 19 Includes index Supt. of Docs. No.: I 19:16:1057 1. Terebratulida, Fossil. 2. Paleontology Triassic. 3. Paleontology The West. I. Title. II. Series: United States Geological Survey Professional Paper 1057 QE797.T29H66 564'.8 77-608314 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03182-5 CONTENTS Page Page Systematic paleontology Continued Abstract ....................... 1 Family Dielasmatidae Continued Introduction .................... 1 Subfamily Dielasmatinae. Previous work................ 1 Rhaetina Waagen ..... Present study ................ 3 Family Terebratulidae ......... 9 Acknowledgments ............ 3 Subfamily Plectoconchiinae. 9 Fossil localities cited in this report. .... 3 Vex, n. gen. ......... 9 Stratigraphic setting of the brachiopods 4 Family Cryptonellidae ......... 11 Faunal relationships. .............. 6 Subfamily Cryptacanthiinae . 11 Biostratigraphic implications........ 6 Obnixia, n. gen. ...... 11 Systematic paleontology............ 7 Family Zeilleriidae ............ 17 Family Dielasmatidae.......... 7 Periallus, n. gen. ......... 17 Subfamily Zugmayeriinae . 7 References cited. ................. 19 Portneufia, n. gen. .... 7 Index ......................... 21 ILLUSTRATIONS [Plates follow index] PLATE 1.
    [Show full text]
  • This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library
    This is a digital document from the collections of the Wyoming Water Resources Data System (WRDS) Library. For additional information about this document and the document conversion process, please contact WRDS at [email protected] and include the phrase “Digital Documents” in your subject heading. To view other documents please visit the WRDS Library online at: http://library.wrds.uwyo.edu Mailing Address: Water Resources Data System University of Wyoming, Dept 3943 1000 E University Avenue Laramie, WY 82071 Physical Address: Wyoming Hall, Room 249 University of Wyoming Laramie, WY 82071 Phone: (307) 766-6651 Fax: (307) 766-3785 Funding for WRDS and the creation of this electronic document was provided by the Wyoming Water Development Commission (http://wwdc.state.wy.us) VOLUME 11-A OCCURRENCE AND CHARACTERISTICS OF GROUND WATER IN THE BIGHORN BASIN, WYOMING Robert Libra, Dale Doremus , Craig Goodwin Project Manager Craig Eisen Water Resources Research Institute University of Wyoming Report to U.S. Environmental Protection Agency Contract Number G 008269-791 Project Officer Paul Osborne June, 1981 INTRODUCTION This report is the second of a series of hydrogeologic basin reports that define the occurrence and chemical quality of ground water within Wyoming. Information presented in this report has been obtained from several sources including available U.S. Geological Survey publications, the Wyoming State Engineer's Office, the Wyoming Geological Survey, and the Wyoming Oil and Gas Conservation Commission. The purpose of this report is to provide background information for implementation of the Underground Injection Control Program (UIC). The UIC program, authorized by the Safe Drinking Water Act (P.L.
    [Show full text]
  • Phosphate Rock in Wyoming
    Phosphate Rock in Wyoming Jacob D. Carnes Report of Investigations No. 68 • 2015 WYOMING STATE GEOLOGICAL SURVEY Thomas A. Drean, Director and State Geologist Director and State Geologist Thomas A. Drean Editing by: Sarah R. Garlick Design and layout by: James R. Rodgers Photomicrograph of phosphate rock from the Poison Creek trench in Lincoln County, Wyo., showing the concentric structure of ap- atite grains commonly found in phosphorites of the Phosphoria Formation. Photomicrograph by Jacob Carnes, 2015. Cover photo: Outcrop of the Meade Peak Member of the Phosphoria Formation along U.S. Hwy 26, approximately 3 miles southwest of Hoback Junction, in Teton County, Wyo. Photo by Jacob Carnes, 2015. Phosphate Rock in Wyoming Wyoming State Geological Survey (WSGS) Report of Investigations No. 68, 2015 Suggested citation: Carnes, J.D., 2015, Phosphate rock in Wyoming: Wyoming State Geological Survey Report of Investigations No. 68, 34 p. The WSGS encourages fair use of its material. We request that credit be expressly given to the “Wyoming State Geological Survey” when citing information from this publication. Please contact the WSGS at 307- 766-2286, ext. 224, or by email at [email protected], if you have any questions about citing materials, preparing acknowledgments, or extensive use of this material. We appreciate your cooperation. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement or approval by the State of Wyoming or the WSGS. Individuals with disabilities who require an alternate form of this publication should contact the WSGS. TTY relay operator 800-877-9975.
    [Show full text]
  • Appendix 1 – Environmental Predictor Data
    APPENDIX 1 – ENVIRONMENTAL PREDICTOR DATA CONTENTS Overview ..................................................................................................................................................................................... 2 Climate ......................................................................................................................................................................................... 2 Hydrology ................................................................................................................................................................................... 3 Land Use and Land Cover ..................................................................................................................................................... 3 Soils and Substrate .................................................................................................................................................................. 5 Topography .............................................................................................................................................................................. 10 References ................................................................................................................................................................................ 12 1 OVERVIEW A set of 94 potential predictor layers compiled to use in distribution modeling for the target taxa. Many of these layers derive from previous modeling work by WYNDD1, 2, but a
    [Show full text]
  • A Preliminary Assessment of Paleontological Resources at Bighorn Canyon National Recreation Area, Montana and Wyoming
    A PRELIMINARY ASSESSMENT OF PALEONTOLOGICAL RESOURCES AT BIGHORN CANYON NATIONAL RECREATION AREA, MONTANA AND WYOMING Vincent L. Santucci1, David Hays2, James Staebler2 And Michael Milstein3 1National Park Service, P.O. Box 592, Kemmerer, WY 83101 2Bighorn Canyon National Recreation Area, P.O. Box 7458, Fort Smith, MT 59035 3P.O. Box 821, Cody, WY 82414 ____________________ ABSTRACT - Paleontological resources occur throughout the Paleozoic and Mesozoic formations exposed in Bighorn Canyon National Recreation Area. Isolated research on specific geologic units within Bighorn Canyon has yielded data on a wide diversity of fossil forms. A comprehensive paleonotological survey has not been previously undertaken at Bighorn Canyon. Preliminary paleontologic resource data is presented in this report as an effort to establish baseline data. ____________________ INTRODUCTION ighorn Canyon National Recreation Area (BICA) consists of approximately 120,000 acres within the Bighorn Mountains of north-central Wyoming and south-central Montana B (Figure 1). The northwestern trending Bighorn Mountains consist of over 9,000 feet of sedimentary rock. The predominantly marine and near shore sedimentary units range from the Cambrian through the Lower Cretaceous. Many of these formations are extremely fossiliferous. The Bighorn Mountains were uplifted during the Laramide Orogeny beginning approximately 70 million years ago. Large volumes of sediments, rich in early Tertiary paleontological resources, were deposited in the adjoining basins. This report provides a preliminary assessment of paleontological resources identified at Bighorn Canyon National Recreation Area. STRATIGRAPHY The stratigraphic record at Bighorn Canyon National Recreation Area extends from the Cambrian through the Cretaceous (Figure 2). The only time period during this interval that is not represented is the Silurian.
    [Show full text]
  • Sequence Stratigraphy and Geochemistry of The
    Report of Investigations 2007-1 SEQUENCE STRATIGRAPHY AND GEOCHEMISTRY OF THE UPPER LOWER THROUGH UPPER TRIASSIC OF NORTHERN ALASKA: IMPLICATIONS FOR PALEOREDOX HISTORY, SOURCE ROCK ACCUMULATION, AND PALEOCEANOGRAPHY by Landon N. Kelly, Michael T. Whalen, Christopher A. McRoberts, Emily Hopkin, and Carla Susanne Tomsich ASK AL A G N S E Y O E L O V G R U IC S A L L A A N SIC D GEOPHY Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2007 Report of Investigations 2007-1 SEQUENCE STRATIGRAPHY AND GEOCHEMISTRY OF THE UPPER LOWER THROUGH UPPER TRIASSIC OF NORTHERN ALASKA: IMPLICATIONS FOR PALEOREDOX HISTORY, SOURCE ROCK ACCUMULATION, AND PALEOCEANOGRAPHY by Landon N. Kelly, Michael T. Whalen, Christopher A. McRoberts, Emily Hopkin, and Carla Susanne Tomsich 2007 This DGGS Report of Investigations is a final report of scientific research. It has received technical review and may be cited as an agency publication. STATE OF ALASKA Sarah Palin, Governor DEPARTMENT OF NATURAL RESOURCES Tom Irwin, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Robert F. Swenson, State Geologist and Acting Director Division of Geological & Geophysical Surveys publications can be inspected at the following locations. Address mail orders to the Fairbanks office. Alaska Division of Geological University of Alaska Anchorage Library & Geophysical Surveys 3211 Providence Drive 3354 College Road Anchorage, Alaska 99508 Fairbanks, Alaska 99709-3707 Elmer E. Rasmuson Library Alaska Resource Library University of Alaska Fairbanks 3150 C Street, Suite 100 Fairbanks, Alaska 99775-1005 Anchorage, Alaska 99503 Alaska State Library State Office Building, 8th Floor 333 Willoughby Avenue Juneau, Alaska 99811-0571 This publication released by the Division of Geological & Geophysical Surveys was produced and printed in Fairbanks, Alaska at a cost of $5.00 per copy.
    [Show full text]
  • Triassic-Jurassic 'Red Beds' of the Rocky Mountain Region": a Discussion
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 1929 "Triassic-Jurassic 'Red Beds' of the Rocky Mountain Region": A Discussion John B. Reeside Jr. U.S. Geological Survey Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Reeside, John B. Jr., ""Triassic-Jurassic 'Red Beds' of the Rocky Mountain Region": A Discussion" (1929). USGS Staff -- Published Research. 498. https://digitalcommons.unl.edu/usgsstaffpub/498 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. The Journal of Geology, Vol. 37, No. 1 (Jan. - Feb., 1929), pp. 47-63 "TRIASSIC-JURASSIC 'RED BEDS' OF THE ROCKY MOUNTAIN REGION": A DISCUSSION' JOHN B. REESIDE, JR. U.S. Geological Survey ABSTRACT The conclusion drawn by Professor E. B. Branson in a recent paper on the "Red Beds" of the Rocky Mountain region that parts of these beds are marine is considered likely. The conclusion that there exists no basis for subdivision of the beds is not accepted, and a division of the Mesozoic part into Lower Triassic, Upper Triassic, and Jurassic units is advocated. The conclusion that no eolian deposits are present likewise is not accepted, and the interpretation of important parts of the Jurassic unit as eolian is advocated. Disagreement is expressed with much of Professor Branson's correlation table, and a substitute is offered.
    [Show full text]
  • 23. Sedimentary History of the Red Sea1
    23. SEDIMENTARY HISTORY OF THE RED SEA1 Peter Stoffers, Laboratorium fur Sedimentforschung, Universitát Heidelberg, Heidelberg, Germany and David A. Ross, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts INTRODUCTION trated is the Miocene evaporites (Frazier, 1970; Lowell and Genik, 1972; Ahmed, 1972) with over 3.8 km penetration Numerous studies have been made of Recent Red Sea in a diapiric area adjacent to the Dahlac Islands (off sediments concerning their paleontology, mineralogy, or Ethiopia) and 3.6 km found overlying basalt off southern geochemistry. In addition, over 50 reports have been Sudan. On the western side of the Red Sea over 1 km of published on the sedimentary environment of the hot brine evaporites was found near the coast of southern Saudi area (21°N) in the central axial valley (see Degens and Ross, Arabia (Gillmann, 1968). Correlations between wells, even 1969, and contained references; Backer and Schoell, 1972). fairly closely spaced ones, generally show marked changes These studies generally indicate considerable climatic in thickness (Carella and Scarpa, 1962), probably due, in fluctuations within the Holocene and Late Pleistocene that part, to salt flowage (Frazier, 1970) or erosional pinch-out are reflected by changes in fauna and sediment along angular unconformities (Ross and Schlee, in press). characteristics. In general, aragonite-cemented lithic layers Most of the wells show unconformities within the Miocene formed during periods of glacially or tectonically lowered section as well as within the post-Miocene sections. stands of sea level when salinity increased in the Red Sea Continuous seismic reflection profiles also show truncations (Milliman et al., 1969).
    [Show full text]
  • Chemostratigraphy Indicates a Relatively Complete Late Permian to Early Triassic Sequence in the Western United States
    Chemostratigraphy indicates a relatively complete Late Permian to Early Triassic sequence in the western United States Matthew R. Saltzman* and Alexa R.C. Sedlacek School of Earth Sciences, The Ohio State University, Columbus, Ohio 43210, USA ABSTRACT Collinson et al. (1976) assigned these beds to the basal “Thaynes” but Although the latest Permian mass extinction and associated δ13C noted that the contact with the underlying Gerster was diffi cult to discern excursion are well documented from the Tethys Ocean, carbonate and lacked relief. The age of the laminated, fenestral, and microgastropod- rocks preserving these events in the eastern Panthalassic Ocean (west- rich beds is controversial. Collinson et al. (1976) and Carr (1981) reported δ13 ern Pangea) are unknown. We present Ccarb from the Gerster and the Triassic (Smithian) conodont Parachirognathus ethingtoni from these Thaynes (Permian and Triassic) Formations in the western United beds in the Confusion Range. However, Wardlaw and Collinson (1986) States and document a negative excursion with no evidence for major later assigned these same basal “Thaynes” beds to the uppermost “Ger- δ13 breaks in continuity. To further constrain the age of the Ccarb excur- ster,” consistent with conodonts they identify as the Permian genus Mer- sion in the absence of index fossils, we analyzed the same samples for rillina in the microgastropod-rich wackestone facies (B. Wardlaw, 2012, 87Sr/86Sr. When examining our new carbon and Sr data in the context personal commun.). Because Merrillina is likely ancestral to Parachirog- of biostratigraphy and sequence stratigraphy, we conclude that parts nathus (Orchard, 2007), taxonomic uncertainty regarding the timing and of the western United States may preserve carbonate successions that morphological defi nition of this transition can explain the discrepancy in span the latest Permian extinction.
    [Show full text]
  • Physical Stratigraphy of the Phosphoria Formation in Northwestern Wyoming
    Physical Stratigraphy of the Phosphoria Formation in Northwestern Wyoming GEOLOGICAL SURVEY BULLETIN 1042-E CONTRIBUTIONS TO ECONOMIC GEOLOGY PHYSICAL STRATIGRAPHY OF THE PHOSPHORIA FORMATION IN NORTHWESTERN WYOMING By Richard P. Sheldon ABSTRACT The rocks of the Ph'osphoria formation in northwestern Wyoming fall into five stratigraphic units, which, from oldest to youngest, are provisionally called the A, B, C, D, and E units. Units A, C, and E are composed dominantly of chert, carbonate rock, and sandstone, whereas units B and D are composed dominantly of mudstone, phosphorite, and dark carbonate rock. Units C and D are con­ tinuous over all of northwestern Wyoming, whereas unit A grades into unit B and unit -E grades into unit D to the southwest. Both units A and B pinch out to the north. With the possible exception of unit A, these units can be recognized in southwestern Montana. Units B, C, and D are. equivalent to the phosphatic phale, Rex, and upper shale .members of the Phosphoria formation in southeastern Idaho. The formation as a whole exhibits a facies change from dominantly chert, mudstone, and phosphorite in the southwestern part of northwestern Wyoming, to dominantly Carbonate rock and sandstone in the northeastern part. The facies change with thinning and pinching out of units and the intergradation of units, " .. - . The rocks of the formation in the area of the report are cyclically deposited. The rock record of a single ideal cycle consists, from base to top, of carbonate rock, chert, phosphorite, chert, and carbonate rock. Sandstone and glauconite in general are found in the carbonate phase of the cycle, whereas mudstone, pyrite,.and organic matter are found in the chert and phosphorite phases of the cycle.
    [Show full text]