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Basement Control on the Development of Selected Michigan Basin Oil and Gas Fields As Constrained by Fabric Elements in Paleozoic Limestones
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 6-1991 Basement Control on the Development of Selected Michigan Basin Oil and Gas Fields as Constrained by Fabric Elements in Paleozoic Limestones Robert Thomas Versical Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Versical, Robert Thomas, "Basement Control on the Development of Selected Michigan Basin Oil and Gas Fields as Constrained by Fabric Elements in Paleozoic Limestones" (1991). Master's Theses. 1010. https://scholarworks.wmich.edu/masters_theses/1010 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. BASEMENT CONTROL ON THE DEVELOPMENT OF SELECTED MICHIGAN BASIN OIL AND GAS FIELDS AS CONSTRAINED BY FABRIC ELEMENTS IN PALEOZOIC LIMESTONES by Robert Thomas Versical A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan June 1991 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. BASEMENT CONTROL ON THE DEVELOPMENT OF SELECTED MICHIGAN BASIN OIL AND GAS FIELDS AS CONSTRAINED BY FABRIC ELEMENTS IN PALEOZOIC LIMESTONES Robert Thomas Versical, M.S. Western Michigan University, 1991 Hydrocarbon bearing structures in the Paleozoic section of the Michigan basin possess different structural styles and orientations. Quantification of the direction and magnitude of shortening strains by applying a calcite twin-strain analysis constrains the mechanisms by which these structures may have developed. -
Cambrian Ordovician
Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation. -
G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine
DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY GEOLOGY OF THE CRAIG QUADRANGLE, ALASKA By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Open-File Report 83-91 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and strati graphic nomenclature Menlo Park, California 1983 Geology of the Craig Quadrangle, Alaska By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Introduction This report consists of the following: 1) Geologic map (1:250,000) (Fig. 1); includes Figs. 2-4, index maps 2) Description of map units 3) Map showing key fossil and geochronology localities (Fig. 5) 4) Table listing key fossil collections 5) Correlation diagram showing Silurian and Lower Devonian facies changes in the northwestern part of the quadrangle (Fig. 6) 6) Sequence of Paleozoic restored cross sections within the Alexander terrane showing a history of upward shoaling volcanic-arc activity (Fig. 7). The Craig quadrangle contains parts of three northwest-trending tectonostratigraphic terranes (Berg and others, 1972, 1978). From southwest to northeast they are the Alexander terrane, the Gravina-Nutzotin belt, and the Taku terrane. The Alexander terrane of Paleozoic sedimentary and volcanic rocks, and Paleozoic and Mesozoic plutonic rocks, underlies the Prince of Wales Island region southwest of Clarence Strait. Supracrustal rocks of the Alexander terrane range in age from Early Ordovician into the Pennsylvanian, are unmetamorphosed and richly fossiliferous, and aopear to stratigraphically overlie pre-Middle Ordovician metamorphic rocks of the Wales Group (Eberlein and Churkin, 1970). -
Michigan Fossils - Student Worksheets – Larger Format – Page 1 of 6
A1 - BRACHIOPOD, invertebrate - A2 - BRACHIOPOD, invertebrate - Pentamerus sp. - Cordell dolomite - Mucrospifier profundus - Silica formation Silurian age - Chippewa Co. - 65 mm, - Devonian age - Washtenaw Co. - 50 mm, internal cast or steinkern - R. Elowski calcite replacement - R. Milstein A3 - TRILOBITE, invertebrate - Phacops A4 - CORAL or COLONIAL CORAL, rana - Silica formation - Devonian age - invertebrate - Syringopora sp. - Cordell Washtenaw Co. - 70 mm, calcite dolomite - Silurian age - Chippewa Co. - replacement - S. Wilson 125 mm, siliceous replacement - R. Milstein Michigan Fossils - Student Worksheets – larger format – page 1 of 6 C1 - MASTODON Tooth, vertebrate - C2 - EUCARYOTIC algae filaments, plant - Mammut americanum - Glacial deposit - Grypania spiralis - Negaunee Iron Quaternary age - 200 mm long, the Formation - Precambrian age - Marquette “Michigan State Fossil” - Central Michigan Co. - large loop about 20 mm , oldest Univ. Rowe Museum macrofossil - GSD C3 - FISH plate, vertebrate - genus not C4 - Septarian nodule - pseudo fossil - - determined - Alpena Limestone - Devonian Ottawa Co. - 75 mm, Looks like a fossil, it age - Alpena Co. - 200 mm at widest point, is not. - S. Wilson calcite replacement - S. Wilson Michigan Fossils - Student Worksheets – larger format – page 2 of 6 E2 - CORAL or COLONIAL CORAL, E1 - CRINOID, invertebrate - Megistocrinus invertebrate - Favosites sp. - Alpena concava - Thunder Bay limestone - Devonian Limestone - Devonian age - Charlevoix Co. - age - Alpena Co. - 30 mm, calcite 100 mm (shown), siliceous replacement - R. replacement - S. Wilson Reszka E3 - BRACHIOPOD, invertebrate - E4 - CEPHALOPOD, invertebrate - Mucrospifler mucronatus - Silica formation - Michelinoceras sp. - Ogontz limestone - Devonian age - Washtenaw Co. - 90 mm, Ordovician age - Alger Co. - 100 mm, calcite replacement - R. Milstein internal cast or steinkern - R. Milstein Michigan Fossils - Student Worksheets – larger format – page 3 of 6 B1 - CORAL or CHAIN CORAL, B2 - CRINOID pieces, invertebrate - invertebrate - Halysites sp. -
Conodonts Frorn the Genesee Formation in Western New York
·U.S: BUREAu Of MINES P.O. BOX 550 IUNEAU, AlASK} OQ9( ' Conodonts frorn the Genesee Formation in Western New York GEOLOGICAL SURVEY PROFESSIONAL PAPER 1032-B \ Conodonts from the Genesee Formation in Western New York By JOHN W. HUDDLE, assisted by JOHN E. REPETSKI STRATIGRAPHY AND CONODONTS OF THE GENESEE FORMATION (DEVONIAN) IN WESTERN AND CENTRAL NEW YORK GEOLOGICAL SURVEY PROFESSIONAL PAPER 1032-B Conodonts from the Genesee Formatz"on z"n western New York, first descrz"bed by G.]. Hz"nde z"n 1879 and W. L. Bryant z·n 1921, are redescrz"bed, and the b£ostrat£graph£c zones are determz"ned UNITED STATES GOVERNMENT PRINTING OFFICE,WASHINGTON 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secreta·ry GEOLOGICAL SURVEY Doyle G. Frederick, Acting Director Library of Congress Cataloging in Publication Data Huddle, John Warfield, 1907-1975 Conodonts from the Genesee Formation in western New York. (Stratigraphy and conodonts of the Genesee Formation (Devonian) in western and central New York) (Geological Survey professional paper ; 1032-B) Bibliography: p. Supt. of Docs. No.: I 19.16:1032-B 1. Conodonts. 2. Paleontology-Devonian. 3. Paleontology-New York (State) I. Title. II. Series. III. Series: United States. Geological Survey. Professional paper ; 1032-B. QE899.H83 557.3'08s [562] 77-608125 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 FOREWORD After John Huddle's death in late November 1975, I was asked to serve as author's representative in the completion of this report. In September 1975, Huddle had completed. -
Traverse City Environmental Assessment 2012
Traverse City Environmental Stewardship Assessment 2012 Let Our Resources Work For You. Workforce • Business • Community Acknowledgements The Northwest Michigan Council of Governments would like to thank all of the people who gave their time and resources towards the development of the City of Traverse City’s Environ- mental Stewardship Assessment. Prepared by: PO Box 506 Traverse City, MI 49685-0506 www.nwm.org With funding from: Financial assistance for this project was provided, in part, by the Michigan Coastal Manage- ment Program, Office of the Great Lakes, Department of Environmental Quality, through a grant from the National Oceanic and Atmospheric Administration, U.S. Department of Com- merce. Michigan's Office of the Great Lakes leads policy development and implements programs to protect, restore and sustain our most precious natural resource. The office collaborates with partners to support sustainable use of these coastal resources, coordinate restoration of severely degraded areas, manage water quality and quantity, prevent aquatic invasive species and engage in emerging issues. We are committed to our Great Lakes mission to ensure a healthy environment, strong economy and high quality of life. 2012 Contents Acknowledgements .................................................................................................................................................. i Contents .................................................................................................................................................................. -
Proceedings of the United States National Museum
THE MIDDLE DEVONIAN TRAVERSE GROUP OF ROCKS IN MICHIGAN, A SUMMARY OF EXISTING KNOWL- EDGE By Erwin R. Pohl Of the Department of Geology, Vanderhilt University, NasJiville, Tenn. INTRODUCTION It has become more and more obvious with the progress of labo- ratory and field studies on the faunas and stratigraphy of the Michi- gan Traverse group of Middle Devonian age that no exact correla- tion between deposits in the eastern and western parts of the State can be established. This conclusion will serve as the focus of major inferential consideration for the discussion that follows, and while the greater portion of this paper will be devoted to the establishment of the stratigraphic sequence of the Traverse Bay area, the truth of the deduction will appear through comparison of this section with the more completely developed group bordering Lake Huron. Newly introduced terms must necessarily be provisional, for the study of this problem in its true light is still in its beginning. Such names are here used merely as a means of clarifying a visualization of the stratigraphic conditions contemporaneous with the deposition. From the standpoint of pure science the most engrossing phase of geological investigation is to the author the derivation of faunas. Marine faunas, so typically encountered in the Traverse, require rational consideration. It appears trite to remark that an associa- tion of shallow water invertebrate species, however long extinct, reacted no more peculiarly to their environment than their livingj representatives. It was an odd individual, not to say species or assemblage, that would walk on dry land or fly through the air from one basin of deposition to another. -
9Th North American Paleontological Convention Abstracts
9th North American Paleontological Convention Abstracts University of Cincinnati Cincinnati, Ohio USA June 21-26, 2009 ISBN 978-1882151127 Copyright ©2009 Cincinnati Museum Center. All rights reserved. Reproduction of the whole or any part of the contents without written permission is prohibited. Sponsored by the University of Cincinnati, The Paleontological Society, The National Science Foundation, The Ohio Geological Survey, The Indiana Geological Society, The Kentucky Geological Survey, BP America, and Cincinnati Museum Center Cincinnati Museum Center 1301 Western Avenue Cincinnati, OH 45203 (513) 287-7000 (800) 733-2077 www.cincymuseum.org Cincinnati Museum Center Scientific Contributions Series Editor – Glenn W. Storrs Graphic Designer – Sherry Stoffer Printed in the United States of America by McNaughton & Gunn, Inc. Dedication NAPC 2009 is dedicated to the memory of Ellis L. Yochelson (1928-2006), principal organizer of the first NAPC (1969) and a major catalyst in its establishment as a highly successful quadrennial meeting. Welcome On behalf of the Associated North American Paleontological Societies, it is my pleasure to welcome you to Cincinnati for the 9th North American Paleontological Convention (NAPC 2009). As the abstracts in this volume attest, this is a wonderfully eclectic meeting, with sessions and presentations covering an array of taxa, and touching on important questions and themes that drive the science of paleontology in the 21st century. In the year when we commemorate the bicentennial of Charles Darwin’s birth and the sesquicentennial of The Origin of Species, it is appropriate that NAPC 2009 take place in Cincinnati. There are few places on the continent that can match the rich paleontological heritage of this region. -
Petrology of the Rockport Quarry Limestone (Middle Devonian Traverse Group) Alpena, Presque Isle and Montmorency Counties, Michigan
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1976 Petrology of the Rockport Quarry Limestone (Middle Devonian Traverse Group) Alpena, Presque Isle and Montmorency Counties, Michigan Charles Willard Cookman Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons, Mineral Physics Commons, and the Sedimentology Commons Recommended Citation Cookman, Charles Willard, "Petrology of the Rockport Quarry Limestone (Middle Devonian Traverse Group) Alpena, Presque Isle and Montmorency Counties, Michigan" (1976). Master's Theses. 614. https://scholarworks.wmich.edu/masters_theses/614 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. PETROLOGY OF THE ROCKPORT QUARRY LIMESTONE (MIDDLE DEVONIAN TRAVERSE GROUP) ALPENA, PRESQUE ISLE AND MONTMORENCY COUNTIES, MICHIGAN by Charles Willard Cookman A Thesis Submitted to the Faculty of the Graduate College in partial fulfillment of the Degree of the Master of Science Western Michigan University Kalamazoo, Michigan December 19 76 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT The basal unit of the dominantly carbonate Traverse Group, the Bell Shale, is gradationally overlain by the Rock- port Quarry Limestone which has a thickness of approximately 14 m. The Rockport Quarry Limestone is composed of a dark unrestricted marine subtidal organic-mud packstone facies, comprised of an algal-mat-bearing coral packstone subfacies and a shallower water crinoid-bryozoan grainstone subfacies; a shoal-forming stromatoporoid biolithite facies; and a la- goonal micrite facies comprised of a subtidal dense subfacies containing gastropods, ostracods, and calcispheres, and an intertidal to supratidal fenestral subfacies. -
American Law and Jurisprudence on Fracing—2012 by Thomas E
American Law and Jurisprudence on Fracing—2012 by Thomas E. Kurth, Michael J. Mazzone, Mary S. Mendoza and Chris S. Kulander The original version of this paper was published by the Rocky Mountain Mineral Law Foundation in the Rocky Mountain Mineral Law Foundation Journal, Vol. 47, No. 2 (2010). This 2012 version represents extensive updates and revisions reflecting new and revised regulations, statutes, and field development nationwide over the last year and a half. (©2012 Haynes and Boone, LLP). i Table of Contents Table of Contents ............................................................................................................................ ii Acknowledgements ......................................................................................................................... 1 Introduction ..................................................................................................................................... 1 Hydraulic Fracturing—an Overview .............................................................................................. 2 Drilling and Groundwater Protection .............................................................................................. 3 Fracing Fluids and Operations ........................................................................................................ 6 Fracing Operations Nationwide ...................................................................................................... 8 Marcellus and Utica Shale ......................................................................................................... -
Smithsonian Miscellaneous Collections Volume 148, Number 2
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 148, NUMBER 2 ffifyarba S. attb Harg Bait* Halrntt THE BRACHIOPOD SUPERFAMILY STENOSCISMATACEA By RICHARD E. GRANT United States Geological Survey (Publication 4569) OS^. C/jp; CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION April 1, 1965 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 148, NUMBER 2 Barkis S. attb ifflan} Baux Maiwti Steward} iFunJn THE BRACHIOPOD SUPERFAMILY STENOSCISMATACEA By RICHARD E. GRANT United States Geological Survey (Publication 4569) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION April 1, 1965 CONNECTICUT PRINTERS, INC. HARTFORD, CONNECTICUT, U.S.A. CONTENTS Page Introduction 1 Type genus 2 Acknowledgments 3 External morphology 4 Size 4 Commissure 4 Plication 6 Costation 7 Stolidium 8 Delthyrium and deltidial plates 13 Internal morphology 14 Camarophorium 14 Spondylium 16 Musculature 18 Hinge plate and cardinal process 22 Crura 22 Lophophore 23 Pallial markings 23 Shell structure 25 Life habits 26 Phylogeny 29 Classification 33 Key 35 Systematics of superfamily Stenoscismatacea 37 Family Atriboniidae 37 Subfamily Atriboniinae 37 Subfamily Psilocamarinae 77 Family Stenoscismatidae 95 Subfamily Stenoscismatinae 95 Subfamily Torynechinae 152 Species doubtfully Stenoscismatacean 160 Genera no longer included in Stenoscismatacea 162 References cited 166 Explanations of plates 175 Index 187 ILLUSTRATIONS PLATES Exp™ Page 1. Atribonium 175 2. Atribonium 175 3. Atribonium 176 4. Sedenticellula, Septacamera, Camarophorinella 176 5. Sedenticellula 177 6. Cyrolexis 177 7. Cyclothyris, Camarophorina 177 8. Camerisma 178 9. Psilocamara, Coledium 178 10. Coledium 179 11. Coledium 179 12. Coledium 179 13. Coledium 180 14. Coledium 180 15. Coledium 180 16. Coledium 181 17. Coledium 181 18. Coledium 182 19. Stenoscisma 182 20. Stenoscisma 183 21. -
Stratigraphic Lexicon for Michigan
Stratigraphic Lexicon for Michigan AUTHORS Paul A. Catacosinos David B. Westjohn [Professor Emeritus, United States Geological Survey Delta College [Associate Professor (Adjunct), University Center, MI 48710] Michigan State University] 1001 Martingale Lane SE 6520 Mercantile Way #6 Albuquerque, NM 87123-4305 Lansing, MI 48911 William B. Harrison, III Mark S. Wollensak, CPG Professor, Department of Geosciences EarthFax Engineering, Inc. Western Michigan University 15266 Ann Drive Kalamazoo, MI 49008 Bath, MI 48808 Robert F. Reynolds Reynolds Geological, L.L.C. 504 Hall Blvd. Mason, MI, 48854 Bulletin 8 Lansing, Michigan, 2001 Geological Survey Division and the Michigan Basin Geological Society State of Michigan John Engler, Govenor Michigan Department of Environmental Quality Russell J. Harding, Director MDEQ Geological Survey Division, P O Box 30256, Lansing, MI 48909-7756 On the Internet @ HTTP://W WW .DEQ.STATE.MI.US/GSD Printed by Authority of Act 451, PA 1994 as amended The Michigan Department of Environmental Quality (MDEQ) will not discriminate Total number of copies printed ........... 1,000 against any individual or group on the basis of race, sex, religion, age, national origin, Total cost: .................................... $2,500.00 color, marital status, disability or political beliefs. Directed questions or concerns to the Cost per copy: ..................................... $2.50 MDEQ Office of Personnel Services, P.O. Box 30473, and Lansing, MI 48909 Page 2 - - Stratigraphic Lexicon for Michigan DEDICATION The authors gratefully dedicate this volume to the memories of Helen M. Martin and Muriel Tara Straight. This volume would not have been possible without their monumental reference work Bulletin 50, An Index of Helen Melville Martin Michigan Geology published by the Michigan Geological Survey in 1956.