DOCSLIB.ORG

Hydrodynamic Character of the Dundee Limestone in the Central Michigan Basin

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Hydrodynamic Character of the Dundee Limestone in the Central Michigan Basin Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 8-1986 Hydrodynamic Character of the Dundee Limestone in the Central Michigan Basin Ann Carol Little Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Hydrology Commons Recommended Citation Little, Ann Carol, "Hydrodynamic Character of the Dundee Limestone in the Central Michigan Basin" (1986). Master's Theses. 1330. https://scholarworks.wmich.edu/masters_theses/1330 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]. HYDRODYNAMIC CHARACTER OF THE DUNDEE LIMESTONE IN THE CENTRAL MICHIGAN BASIN by Ann Carol Little 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 August 1986 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. HYDRODYNAMIC CHARACTER OF THE DUNDEE LIMESTONE IN THE CENTRAL MICHIGAN BASIN Ann Carol Little Western Michigan University, 1986 The Middle Devonian Dundee Limestone underlies most of the Lower Peninsula of Michigan. A potentiometric surface constructed of the formation, utilizing pressure data was compared to local and regional structure, permeability trends, specific gravity of the brines, oil accumulations, and surficial topography. The data were distributed mainly in the central basin area, with information becoming more sparse around the basin margins. This created difficulties in the determination of the extent of control imparted by each of the factors, in flow direction. Surficial topography, on a regional scale, is likely the most influential of the controls, with the Dundee Limestone brines flowing toward outcrops in Lake Michigan. Lake Michigan is acting as a potentiometric low. Lack of data in the eastern portion of the state resulted in a lack of definition of the potentiometric surface in this area; therefore, no relationship could be determined between flow direction and Lake Huron. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ACKNOWLEDGEMENTS This research was supported in part by a research grant from Western Michigan University Graduate College. I am grateful for the encouragement given to me by Dr. W. Thomas Straw throughout the study and his helpful comments during the preparation of the manuscript. Thanks are also due to Dr. Richard N. Passero and Dr. William B. Harrison III for their reading and constructive criticism of the final drafts. I would also like to thank Dr. John D. Grace for his support and insight/ and Norman Grannemann of the U.S.G.S. for some valuable literature. Special thanks go to my family for their belief in my abilities, to Steve for his constant encouragement, and to all my friends of the department for making this journey more bearable. Ann Carol Little Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. University Microfilms International r : / IlidJ" Itt 1.0 “ •— U133.2 22 144L. EsaB36 2.0 u l.l 1.8 1-25 I U 116. MICROCOPY RESOLUTION TEST CHART NATIONAL BUREAU OF STANDARDS STANDARD REFERENCE MATERIAL 1010a (ANSI and ISO TEST CHART No. 2) "V . University Microfilms Inc. 300 N. Zeeb Road, Ann Arbor, MI 48106 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. INFORMATION TO USERS This reproduction was made from a copy of a manuscript sent to us for publication and microfilming. While the most advanced technology has been used to pho­ tograph and reproduce this manuscript, the quality of the reproduction is heavily dependent upon the quality of the material submitted. Pages in any manuscript may have indistinct print. In all cases the best available copy has been filmed. The following explanation of techniques is provided to help clarify notations which may appear on this reproduction. 1. Manuscripts may not always be complete. When it is not possible to obtain missing pages, a note appears to indicate this. 2. When copyrighted materials are removed from the manuscript, a note ap­ pears to indicate this. 3. Oversize materials (maps, drawings, and charts) are photographed by sec­ tioning the original, beginning at the upper left hand comer and continu­ ing from left to right in equal sections with small overlaps. Each oversize page is also filmed as one exposure and is available, for an additional charge, as a standard 35mm slide or in black and white paper format.* 4. Most photographs reproduce acceptably on positive microfilm or micro­ fiche but lack clarity on xerographic copies made from the microfilm. For an additional charge, all photographs are available in black and white standard 35mm slide format.* *For more information about black and white slides or enlarged paper reproductions, please contact the Dissertations Customer Services Department. T Dissertation LJ 1VJL1 Information Service University Microfilms International A Bell & Howell Information Company 300 N. Zeeb Road, Ann Arbor, Michigan 48106 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. 1328537 Little, Ann Carol HYDRODYNAMIC CHARACTER OF THE DUNDEE LIMESTONE IN THE CENTRAL MICHIGAN BASIN Western Michigan University M.S. 1986 University Microfilms International300 N. Zeeb Road, Ann Arbor, Ml 48106 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS ACKNOWLEDGEMENTS .................................. ii LIST OF FIGURES .................................. v LIST OF P L A T E S ..................................... vii INTRODUCTION ...................................... 1 Study Area Location ........................... 3 Literature Review ............................. 3 REGIONAL GEOLOGY .................................. 8 Stratigraphy .................................... 12 Devonian Strata ............................. 12 Dundee Limestone ......................... 15 REGIONAL STRUCTURE ............................... 22 Central Michigan Structure .................... 25 Dundee Structure ........................... 25 THE CONCEPT OF POTENTIAL ........................... 29 Potential Energy .......................... 29 The Potentiometric Surface .................... 34 Tilted Oil-Water Contacts .................. 37 Drillstem Tests ............................... 39 Pressure Charts ............................. 41 Incomplete Drillstem Records ............. 44 Brine D a t a ......................................... 45 INVESTIGATIVE METHODS ............................. 49 Drillstem Test Classification .................. 49 iii Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Table of Contents— Continued Pressure-Depth Gradient Diagrams .......... 52 Calculation of H laM>..............................54 Permeability Trends ........................... 55 Structure Contour Map ......................... 57 RESULTS ................................................58 Drillstem Classification Results ............. 58 Specific Gravity Results ...................... 64 Specific Gravity Trends...................... 68 Permeability Trends ........................... 70 Relation to Potential Gradient ........... 71 Structural Relationships ....................... 71 Effect of Topography ........................... 72 CONCLUSIONS ........................................... 76 APPENDICES A. Drillstem Test and Bottom-Hole Pressure D a t a ................................ 80 B. Brine D a t a .................................... 83 BIBLIOGRAPHY ...................................... 85 iv Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. LIST OF FIGURES 1. Study Area Location ......................... 4 2. Structural Features Associated With the Michigan B a s i n ........... *. ........... 9 3. Generalized Geologic and Tectonic Map of the Michigan Basin ....................... 11 4. Generalized Stratigraphic Column of the Michigan B a s i n ......................... 13 5. Thickness-Lithofacies Map of the Dundee Limestone ........................... 18 6. Major Fold Trends of the Michigan Basin ...................................... 23 7. Structure Map on the Dundee Limestone . 26 8. Cross-Section of the Michigan .............. 27 9. Model illustrating Potential Energy Minimums and Barriers ....................... 32 10. Typical Drillstem Test String .............. 40 11. Pressure-Response Curve from Drillstem T e s t ......................................... 42 12. Contour Map of Equal Static Head in the Marshall Sandstone .................... 47 13. Pressure-Depth Gradient Plot for Various Fluids ............................. 53 14. Pressure-Depth Gradient Plot for Dundee Brines ................................ 59 15. Potentiometric Surface of the Dundee
Load more

Recommended publications
  • A Summary of Petroleum Plays and Characteristics of the Michigan Basin
    DEPARTMENT OF INTERIOR U.S. GEOLOGICAL SURVEY A summary of petroleum plays and characteristics of the Michigan basin by Ronald R. Charpentier Open-File Report 87-450R This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Denver, Colorado 80225 TABLE OF CONTENTS Page ABSTRACT.................................................. 3 INTRODUCTION.............................................. 3 REGIONAL GEOLOGY.......................................... 3 SOURCE ROCKS.............................................. 6 THERMAL MATURITY.......................................... 11 PETROLEUM PRODUCTION...................................... 11 PLAY DESCRIPTIONS......................................... 18 Mississippian-Pennsylvanian gas play................. 18 Antrim Shale play.................................... 18 Devonian anticlinal play............................. 21 Niagaran reef play................................... 21 Trenton-Black River play............................. 23 Prairie du Chien play................................ 25 Cambrian play........................................ 29 Precambrian rift play................................ 29 REFERENCES................................................ 32 LIST OF FIGURES Figure Page 1. Index map of Michigan basin province (modified from Ells, 1971, reprinted by permission of American Association of Petroleum Geologists)................. 4 2. Structure contour map on top of Precambrian basement, Lower Peninsula
    [Show full text]
  • 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]
  • 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]
  • 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.
    [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]
  • Columnals (PDF)
    2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown.
    [Show full text]
  • Middle Devonian Formations in the Subsurface of Northwestern Ohio
    STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone ..........................
    [Show full text]
  • Bathyurus Perplexus Billings, 1865: Distribution and Biostratigraphic Significance
    Current Research (2020) Newfoundland and Labrador Department of Natural Resources Geological Survey, Report 20­1, pages 1­27 BATHYURUS PERPLEXUS BILLINGS, 1865: DISTRIBUTION AND BIOSTRATIGRAPHIC SIGNIFICANCE W.D. Boyce Regional Geology Section ABSTRACT The type specimen of Bathyurus perplexus Billings is a pygidium (GSC 632) from faulted limestone exposed in East Arm, Bonne Bay, Gros Morne National Park (Gros Morne – NTS 12H/12). Some workers have regarded it as a junior subjective synonym of B. extans (Hall); others have compared it to Acidiphorus pseudobathyurus Ross. The discovery of additional scle­ rites (cranidia, librigenae, thoracic segments, pygidia) confirms its distinctness. Bathyurus perplexus is widespread in west­ ern Newfoundland; it has a restricted stratigraphic range and is the nominate species of the Bathyurus perplexus Biozone. It occurs in dolostones or dolomitic lime mudstones of the uppermost Aguathuna Formation (St. George Group) at Table Point (Bellburns – NTS 12I/06 and 12I/05); in Back Arm, Port au Choix (Port Saunders – NTS 12I/11); Big Spring Inlet (St. Julien’s – NTS 02M/04); and on the Radar Tower Road, Table Mountain (Stephenville – NTS 12B/10). It also occurs in the immedi­ ately overlying Spring Inlet Member of the basal Table Point Formation (Table Head Group) in the Phillips Brook Anticline (Harrys River – NTS 12B/09); and at Table Point (Bellburns – NTS 12I/06 and 12I/05). Bathyurus perplexus is associated with conodont Assemblage VII of Stait and Barnes, which indicates a correlation with the Anomalorthis (brachiopod) Biozone of the Whiterockian, Kanoshian Stage, i.e., early Middle Ordovician, Darriwilian. Typically, it is associated with shallow­ water (littoral) Midcontinent Province conodonts and leperditicopid ostracodes (Bivia), an assemblage characteristic of the long­ranging, low­diversity, nearshore Bathyurus Biofacies.
    [Show full text]
  • Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1990 Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan Brendan Ciaran Curran Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Curran, Brendan Ciaran, "Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan" (1990). Master's Theses. 1053. https://scholarworks.wmich.edu/masters_theses/1053 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]. RESERVOIR GEOLOGY OF THE DUNDEE LIMESTONE, WEST BRANCH FIELD, MICHIGAN by Brendan Ciaran Curran 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 December 1990 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. RESERVOIR GEOLOGY OF THE DUNDEE LIMESTONE, WEST BRANCH FIELD, MICHIGAN Brendan Ciaran Curran, M.S. W estern Michigan University, 1990 West Branch field is a low-relief, NW-SE-trending anticline near the center of the Michigan basin. Since 1934, the Dundee Limestone (Middle Devonian) has produced over 12 million barrels of oil from this field. From core studies, six depositional facies types were recognized in the Dundee. These are dominated by bioclastic carbonate sand facies deposited in normal- marine shelf settings. Although burial cements have occluded some porosity, carbonate sand facies have retained significant primary interparticle porosity and are the most important reservoir rocks.
    [Show full text]
  • Detroit River Group in the Michigan Basin
    GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan.
    [Show full text]
  • The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
    International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A.
    [Show full text]
  • Geological Controls on Stratigraphy and Sedimentation of the Mississippian Marshall Formation, Michigan Basin, U.S.A
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 8-2015 Geological Controls on Stratigraphy and Sedimentation of the Mississippian Marshall Formation, Michigan Basin, U.S.A. Joseph G. Adducci Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons, Geomorphology Commons, and the Sedimentology Commons Recommended Citation Adducci, Joseph G., "Geological Controls on Stratigraphy and Sedimentation of the Mississippian Marshall Formation, Michigan Basin, U.S.A." (2015). Master's Theses. 617. https://scholarworks.wmich.edu/masters_theses/617 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]. GEOLOGICAL CONTROLS ON STRATIGRAPHY AND SEDIMENTATION OF THE MISSISSIPPIAN MARSHALL FORMATION, MICHIGAN BASIN, U.S.A by Joseph G. Adducci A thesis Submitted to the Graduate College in partial fulfillment of the requirements for the degree of Master of Science Geosciences Western Michigan University August 2015 Thesis Committee: David A. Barnes, Ph.D. (Chair) William B. Harrison, III, Ph.D. Peter J. Voice, Ph.D. GEOLOGICAL CONTROLS ON STRATIGRAPHY AND SEDIMENTATION OF THE MISSISSIPPIAN MARSHALL FORMATION, MICHIGAN BASIN, U.S.A. Joseph G. Adducci, M.S. Western Michigan University, 2015 An understanding of regional orogenic, climatic, and eustatic processes is critical to the interbasinal correlation of Paleozoic strata in eastern North America. Tectonic activity associated with the culmination of Appalachian Orogenic events has been shown to have regional influence on paleostructure and sediment dispersal in the Appalachian foreland basin and adjacent intracratonic Illinois and Michigan basins.
    [Show full text]