History and Performance of the Coldwater Oil Field, Michigan

Total Page:16

File Type:pdf, Size:1020Kb

History and Performance of the Coldwater Oil Field, Michigan HISTORY and PERFORMANCE of the COLDWATER OIL FIELD, MICHIGAN Downloaded from http://onepetro.org/jpt/article-pdf/6/02/23/2238397/spe-278-g.pdf by guest on 30 September 2021 C. R. CRISS SOHIO PETROLEUM CO. MEMBER AIME OKLAHOMA CITY, OKLA. R. l. McCORMICK T.P.3748 ABSTRACT tion in the west central part of the Michigan basin. Except as influenced by the extent of closure and the Thi~' paper summarizes the development and perform· thickness of the oil column, reservoir performance is ance of the Coldwater Oil field, Isabella County. Mich. believed to be representative of Rogers City fields in Production is obtained at a depth of 3750 ft from a this part of the basin. For this reason, it is felt that dolomite reservoir, which is probably both Rogers City the following presentation of factual data for the field and Dundee. There appears to be no persistent barrier will be of general interest. to vertical fluid movement between the Rogers City and Dundee, and both formations are believed to have a common original oil-water contact. No wells are open HISTOR Y AND DEVELOPMENT to production at the level of the Dundee. The discovery of the field in 1944 was followed by Discovery of the Coldwater field during Aug., 1944, the drilling of 81 producing wells and nine dry holes. followed favorable subsurface geological correlations By the end of 1952, the field had produced 12,763,000 and core tests drilled to a shallow stratigraphic marker bbl of oil, at which time 69 active wells were producing horizon. The field is located in the west central part 3600 BID oil and 21,000 BID water. of the Michigan Basin in Coldwater Township (TI6N­ The reservoir has an effective natural water drive, R6W), Isabella County. It is 60 miles west-northwest and bottom-hole pressure has declined 75 psi from an of Bay City, and near the geographic center of the original pressure of 1453 psi. Oil is undersaturated at southern peninSUla of Michigan. The discovery well reservoir conditions with a solution GOR of 512 cu flowed 200 bbl of oil the first 24 hours from the ftlbbl and a saturation pressure of 1190 psi. Rogers City dolomite at a depth of approximately 3750 ft. Field production is principally from the Rogers City with a minor amount assumed to come from the under­ INTRODUCTION lying Dundee dolomite, although none of the wells are open to production at the level of the Dundee. Both Although the Coldwater Field is now in its ninth the Rogers City and Dundee formations belong to year of production, it ranks seventh in cumulative the Devonian system (See Geologic Column-Fig. 1.) recovery, and second in current daily oil production In addition to Rogers City-Dundee oil production, in the State. Following complete development of the sweet gas is produced from the Michigan Stray sand field in 1946, it has consistently contributed approxi­ of the Mississippian system at a depth of 1400 ft. The mately 11 per cent of Michigan's daily production. gas reservoir has approximately the same areal extent Coldwater appears to have a greater pay thickness as the underlying oil reservoir. Although gas production than most fields producing from the Rogers City forma- is an important feature of the Coldwater field, this report is concerned only with the oil reservoir. Manuscript received in the Petroleum Branch office Aug 17. 1953. Paper presented at the Petroleum Branch Fall Meeting in Dallas, The productive area is approximately 3200 acres. The Tex., Oct. 18-21, 1953. pool is developed on a 40 acre spacing pattern with Discussion of this and all following technical papers is invited. Discussion in writing (3 copies) may be sent to the offices of the wells drilled in the center of the north half of 40 acre Journal of Petroleum Technology. Any discussion offered after Dec. 31, 1954, should be in the form of a new paper. tracts, except for a few off-pattern wells drilled along Trans. AIME SPE 278-G FEBRUARY, 1954 • JOURNAL OF PETROLEUM TECHNOLOGY· • 23 SYSTEM FORMATION LITHOLOGY DEPTH Since the Rogers City-Dundee has an active water PLEISTOCENE GLACIAL DRIFT SAND, GRAVEL, CLAY 0-550 drive, oil production has been accompanied by steadily PENNSYLVANIAN SAGINAW GYPSUM 550-850 increasing water production rates. There has been a RED CLAY SHALE, SANDSTONE slight drop in reservoir pressure; however, it has re­ PARMA SANDSTONE 850-1000 mained above saturation pressure. MISSISSIPPIAN BAYPORT LIMESTONE. SOME SANDSTONE 1000-1100 Daily oil and water production rates, cumulative oil DOLOMITE production, number of producing wells and reservoir MICHIGAN SHALE, ANHYDRITE . 1100-1500 SANDSTONE, LENSES (GAS) pressure are plotted versus time on Fig. 2. WHITE SANDSTONE 1500-1700 RED SANDSTONE COLDWATER GRAY SHALE 1700-2500 COLDWATER OIL RESERVOIR MISSISSIPPIAN SUNBURY- BEREA- BEDFORD BROWN SHALE 2500- 3100 & DEVONIAN & ANTRIM (UNDIFFERENTIATED) STRUCTURE DEVONIAN TRAVERSE GROUP LIMESTONE 3100-3650 LIMY SHALE IN LOWER PARTS Fig. 3 shows the Rogers City structure to be an BELL SHALE GRAY SHALE, LIM"!' IN BASE 3650-3700 irregularly shaped, gently rounded dome. It is located ROGERS CITY BROWN S(CONDAi<Y DOLOMITE 3700-3i3~ 15 to 20 miles west of the center of the synclinal axis DUNDEE TAN PRIMARY DOLOMITE of the Michigan basin. Regional dip is to the northeast, FIG. 1 - GEOLOGIC COLUMN, COLDWATER FIELD. and, the steepest dips of the Coldwater structure are found along the northeast side of the field with slightly lesser dips toward synclinal re-entrants along the north the edge of the producing area. A total of 81 pro­ and south sides of the field. The structure has two Downloaded from http://onepetro.org/jpt/article-pdf/6/02/23/2238397/spe-278-g.pdf by guest on 30 September 2021 ducing wells and nine dry holes have been drilled with axes, the major axes trending northwest-southeast, and development substantially completed by the end of the minor axes trending northeast-southwest. 1946. Subsequent to 1946, seven producing wells and two dry holes were drilled on the extreme edges of PAY ZONES the field. Oil production rates have been regulated since dis­ Long standing usage by the oil industry of the term covery of the field. The total field allowable was 4600 "Dundee," to include both the Rogers City and Dundee BID at the end of 1946 when development was sub­ formations, has resulted in "Rogers City" being an stantially complete, and has varied up to 6700 BID. unfamiliar term to many who are well acquainted with Except as influenced by allowable changes, by the end its contents and characteristics. This usage developed of 1952 oil production had declined slowly to 3600 BID since, in many areas, the contact between these forma­ and water production increased from 1800 B/D to tions could not easily be determined from cable tool 21,000 BID. At this time cumulative production was cuttings. With continuing oil development plus a few 12,763,000 bbl of oil and 25,800,000 bbl of water, and rotary cores in the Central Michigan basin and quarry­ there were 69 active producing wells. ing operations in outcrops on the rim of the basin, it 0 22 f 150 :> ~ ~ ) el45 0 -.......... 20 "v; t---.. BOTTOM HOLE PRESSURE r~ 0. I r-- i ~140 0 rL In! I <D r-- P-TI <3 -- I - ::I~ ~ i a: 0 I I 6 ~ 80 ~" 135 ! i:: I '" I 7 ~ :i U o ~ 1300 l.r : ~ ~ I 4 0"' 70 ~ t---' u Z NUMBER PRODUCING W,LLS r- In r-' I ,.1 U ~ ~ I o IU I x ~) ALLOWABLE CHA~ I ! 2 r v I 2 ~ 60 j.J I z ,.1 \..r tL. Ii--- r ./v o -' ~ '"-' 'flcLr' ~ I : in ALLOWABLE CHANGE /'" w 0 I o 50 :. I I ~ If ~ I-'1..n I \ .- / "": a: u ~_• .J ,;;:;: w ::> r ........... [7 ~ ~ o 6 ~ 8 ~ 400 f1-I DAILY OIL PRODUCTION r ~ g: z ./v r r" f------ h- ::l ~ ~ o o "u v~ a: ~ a: o 3 I Inl 6 'U 1.// " 30 ~ ,IT CUMULATIVE OIL PRODUCTION :> ~ ::> r _1- /W z 1(; 4 /0 4 20 J /' Vn. I~ v ...... 2 /" 1\ 10 DAIL Y I WATER PRODICTION f-r v 'r- 1 f-..-""" 0 1.rJ ~ o 1944 -I 9 4 ~ 1946 194 "I I I 948 I 1949 19 SO 1951 19 5 2 19 oS 3 FIG. 2 - DEVELOPMENT, PRODUCTION RATES AND PERFORMANCE DATA, ROGERS CITY - DUNDEE RESERVOIR, COLDWATER FIELD. 24 •• JOURNAL OF PETROLEUM TECHNOLOGY· FEBRUARY, 1954 Trans. AIME L E Co f. N 0 Core data at Coldwater was limited to two wells £&$... L'f W",TER OI$f>O$"'I,..WELL$ cored with conventional barrels. Matrix porosity meas­ f!i!:, .... S ... NQONED S"'I.T WA.TER DISPOS"'I,. WELLS I urements average 4.2 per cent for 39 Rogers City core plugs, and 2.5 per cent for 16 Dundee core plugs. The i I - contribution of vugs to the effective porosity in the :- I ' t/: Rogers City is unknown but probably is appreciable. The I 1/· '<\ ~ ~ m,1. V.L¥ v contribution of vugs to Dundee porosity is also un­ 1 (~ --- - r 0~~",+--, known but probably is negligible, or at least much less .-~ .. <~~ than in Rogers City. Horizontal permeabilities ranged /..// from zero to 1368 md and vertical permeabilities from ~ (1 1( T r--"" I zero to 62 md. N Forty-five ft were cored at one well with 84 per cent I:I '~ ,~'l i Ii .1. '~0--~ '~r'~ '-:::::~i':' ~ recovery and 48 ft cored at the other well with 83 . D'\~\ ,\ \ per cent recovery. The lost section at both wells is < ./::::r~ presumed to have been vugular sections too fragile to \~~II' .,30 I~ 3> 17~;' lV V.
Recommended publications
  • 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]
  • 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]
  • 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]
  • IC-39 Geology and Ground Water Resources of Floyd and Polk
    INFORMATIONCIRCULAR~ ~ GEOLOGY AND GROUND-WATER RESOURCES OF FLOYD AND POLK COUNTIES, GEORGIA by Charles W. Cressler THE GEOLOGICAL SURVEY OF GEORGIA DEPARTMENT OF MINES, MINING AND GEOLOGY Jesse H. Auvil, Jr. State Geologist and Director ATLANTA 1970 For convenience in selecting our reports from your bookshelves, they will be color-keyed across the spine by subject as follows: Red Valley & Ridge mapping and structural geology Dk. Purple Piedmont & Blue Ridge mapping and struc- tural geology Maroon Coastal Plain mapping and stratigraphy Lt. Green Paleontology Lt. Blue Coastal Zone studies Dk. Green Geochemical and Geophysical studies Dk. Blue Hydrology Olive Economic geology Mining directory Yellow Environmental studies Engineering studies Dk. Orange Bibliographies and lists of publications Brown Petroleum and natural gas Black Field trip guidebooks. Colors have been selected at random, and will be aug­ mented as new subjects are published. GEOLOGY AND GROUND-WATER RESOURCES OF FLOYD AND POLK COUNTIES, G EORG IA by Charles W. Cressler THE GEOLOGICAL SURVEY OF GEORGIA DEPARTMENT OF MINES, MINING AND GEOLOGY PREPARED IN COOPERATION WITH THE U.S. GEOLOGICAL SURVEY ATLANTA 1970 CONTENTS Page No. Abstract . 1 Introduction 1 Location and extent of area . 1 Physiography, topography, and climate 2 Purpose, scope, and methods of investigation 2 Well and spring numbering system 3 Previous investigations . 3 Acknowledgments . 3 Geologic formations and their water-bearing properties 4 Cambrian System . 4 Shady Dolomite 4 Rome Formation . 6 Conasauga Formation 9 Cambro-Ordovician Sediments . 13 Knox Group ..... 13 Copper Ridge Dolomite 13 Chepultepec Dolomite . 13 Longview Limestone 13 Ordovician System . 16 Newala Limestone 16 Lenoir Limestone 20 Mosheim Member 20 Deaton Member 22 Rockmart Slate 23 Other formations of Ordovician age .
    [Show 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.
    [Show full text]
  • Possible Salt Mine and Brined Cavity Sites for Radioactive
    <1 ORNL/Sub/7010-1 POSSIBLE SALT MINE AND BRINED CAVITY SITES FOR : , n RADIOACTIVE WASTE DISPOSAL IN THE NORTHEASTERN (;'' 1 SOUTHERN PENINSULA OF MICHIGAN Kenneth K. Landes Consulting Geologist Ann Arbor, Michican and Harold L. Bourne Consulting Geologist Northville, Michican \ May 31, 1976 - - : if,- V ' A ^ v;, . • v This report was prepared by Kenneth K. Landes and v 1-, •• . I'-1 r. ' i •. , . • V", Harold L. Bourne under Consultant Subcontract 7010 • V\ I V'.l. ; , -v. , with Union Carbide Corporation, Nuclear Division. The subcontract was administered by Oak Ridge Natior/al Laboratory. - v''*'' v.'-1: QFFICE OF" WASTE! ISOLATION >y:>; \ ^ OAK RIDGE. TENNESSEE t f prepared for the U.S. ENERGY RESEARCH AND DEVELOPMENT ADMINISTRATION under U.S. GOVERNMENT Contract W-7405 eng 26 This informal document contains information which is preliminary and may be fragmentary or of limited scope. The assumptions, views, and conclusions expressed in I V' this document are those of the authors and are not to be interpreted as those of Union Carbide Corporation, Nuclear Division, or liSERDA. DISTRIBUTION OF THIS DOCUMENT IS UNLIMITED POSSIBLE SALT MINE AND BRINED CAVITY SITES FOR RADIOACTIVE WASTE DISPOSAL IN THE NORTHEASTERN SOUTHERN PENINSULA OP MICHIGAN Second Edition by Kenneth K. Landes, Consulting Geologist, Ann Arbor MI assisted by Harold L. Bourne Consulting Geologist, Northville, MI Report prepared for Union Carbide Corporation, Nuclear Div., Energy, Research, and Development Administration, Oak Ridge, TN Subcontract 7010 31 May 1976 -
    [Show full text]
  • University of Michigan University Library
    CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 24, No. 11, p. 119-123 (1 text-fig.) OCTOBER4, 1973 PALEOECOLOGICAL INTERPRETATION OF THE ROGERS CITY LIMESTONE (MIDDLE DEVONIAN, NORTHEASTERN MICHIGAN) BY ROBERT M. LINSLEY Colgate University, Hamilton, New York 13346 MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: ROBERTV. KESLING The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48104. VOLS.2-23. Parts of volumes may be obtained if available. Price lists available upon inquiry. VOLUME24 1. A new species of Porocrinus from the Middle Ordovician Kimmswick Limestone of Missouri, by Robert V. Kesling. Pages 1-7, with 2 plates and 8 text-figures. 2. Strataster devonicus, a new brittle-star with unusual preservation from the Middle Devonian Silica Formation of Ohio, by Robert V. Kesling. Pages 9-15, with 2 plates and 3 text-figs. 3. Coccoliths and related calcareous nannofossils from the Upper Cretaceous Fencepost Limestone of northwestern Kansas, by John M. Huh and Charles I. Smith. Pages 17-22, with 2 plates. 4. Ordovician vertebrates from Ontario, by Kathleen Anne Lehtola.
    [Show full text]
  • Report of Investigation 15 SUBSURFACE GEOLOGY of BARRY COUNTY, MICHIGAN
    Geological Survey Ordovician System .......................................................10 Report of Investigation 15 Cincinnatian Series...................................................10 Trenton Group ..........................................................10 SUBSURFACE GEOLOGY OF BARRY COUNTY, Black River Group ....................................................10 MICHIGAN St. Peter Sandstone .................................................11 by Prairie du Chien Group.............................................11 Richard T. Lilienthal Cambrian System.........................................................11 Illustrations by Author Trempealeau Formation ...........................................11 Lansing Munising Formation ..................................................12 1974 STRUCTURAL GEOLOGY .............................................12 POROUS INTERVALS....................................................12 Contents REFERENCES AND FURTHER READING ...................16 FOREWORD......................................................................2 ABSTRACT .......................................................................2 Illustrations INTRODUCTION ...............................................................3 GEOLOGIC SETTING.......................................................3 Figures MINERAL RESOURCES...................................................3 Index map ...................................................................................2 Surface Minerals ............................................................3
    [Show full text]
  • Application of Well Log Tomography to the Dundee and Rogers City Limestones, Michigan Basin, USA
    Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Dissertations, Master's Theses and Master's Reports - Open Reports 2004 Application of well log tomography to the Dundee and Rogers City Limestones, Michigan Basin, USA Mellisa A. Le M. Michigan Technological University Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geology Commons Copyright 2004 Mellisa A. Le M. Recommended Citation Le, Mellisa A. M., "Application of well log tomography to the Dundee and Rogers City Limestones, Michigan Basin, USA", Master's Thesis, Michigan Technological University, 2004. https://doi.org/10.37099/mtu.dc.etds/328 Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geology Commons APPLICATION OF WELL LOG TOMOGRAPHY TO THE DUNDEE AND ROGERS CITY LIMESTONES, MICHIGAN BASIN, USA By Mellisa A. Le A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Geological Engineering MICHIGAN TECHNOLOGICAL UNIVERSITY 2004 This thesis, “Application of Well Log Tomography to the Dundee and Rogers City Limestones, Michigan Basin, USA” is hereby approved in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in the field of Geological Engineering. Department of Geological and Mining Engineering and Sciences Signatures: Thesis Advisor: James R. Wood Department Chair: Wayne D. Pennington Date: Abstract The Michigan Basin is located in the upper Midwest region of the United States and is centered geographically over the Lower Peninsula of Michigan. It is filled primarily with Paleozoic carbonates and clastics, overlying Precambrian basement rocks and covered by Pleistocene glacial drift.
    [Show full text]
  • 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.
    [Show full text]