Chapter 1: Introduction
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Stratographic Coloumn of Iowa
Iowa Stratographic Column November 4, 2013 QUATERNARY Holocene Series DeForest Formation Camp Creek Member Roberts Creek Member Turton Submember Mullenix Submember Gunder Formation Hatcher Submember Watkins Submember Corrington Formation Flack Formation Woden Formation West Okoboji Formation Pleistocene Series Wisconsinan Episode Peoria Formation Silt Facies Sand Facies Dows Formation Pilot Knob Member Lake Mills Member Morgan Member Alden Member Noah Creek Formation Sheldon Creek Formation Roxana/Pisgah Formation Illinoian Episode Loveland Formation Glasford Formation Kellerville Memeber Pre-Illinoian Wolf Creek Formation Hickory Hills Member Aurora Memeber Winthrop Memeber Alburnett Formation A glacial tills Lava Creek B Volcanic Ash B glacial tills Mesa Falls Volcanic Ash Huckleberry Ridge Volcanic Ash C glacial tills TERTIARY Salt & Pepper sands CRETACEOUS "Manson" Group "upper Colorado" Group Niobrara Formation Fort Benton ("lower Colorado ") Group Carlile Shale Greenhorn Limestone Graneros Shale Dakota Formation Woodbury Member Nishnabotna Member Windrow Formation Ostrander Member Iron Hill Member JURASSIC Fort Dodge Formation PENNSYLVANIAN (subsystem of Carboniferous System) Wabaunsee Group Wood Siding Formation Root Formation French Creek Shale Jim Creek Limestone Friedrich Shale Stotler Formation Grandhaven Limestone Dry Shale Dover Limestone Pillsbury Formation Nyman Coal Zeandale Formation Maple Hill Limestone Wamego Shale Tarkio Limestone Willard Shale Emporia Formation Elmont Limestone Harveyville Shale Reading Limestone Auburn -
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. -
Long-Range Petroleum Migration in the Illinois Basin CRAIG M
ILLINOIS STATE GEOLOGICAL SURVEY Interior Cratonic Basins, 1991, edited by Reprint Series 1991 - T26 M. W. Leighton, D. R. Kalata, D. F. Oltz, and J. J. Eidel: American Association of Petroleum Geologists Memoir 51,819 p. CHAPTER 26 Long-Range Petroleum Migration in the Illinois Basin CRAIG M. BETHKE DONALD F. OLTZ University of Illinois Illinois State Geological Survey Urbana, Illinois Champaign, Illinois JACKIE D. REED ARCO Oil and Gas Company Plano, Texas Editor's note: No treatment of oil and gas in the Illinois In this section, we define the migration that has basin would be complete without an overview of occurred in the Illinois basin on the basis of shale hydrocarbon migration. The following is a condensed petrographic observations and geochemical correla version, made especially for this volume, of an article tions. We emphasize the origin of oils found in shallow that will appear in the American Association of reservoirs, mostly in Silurian strata to the north and Petroleum Geologists Bulletin in 1991. northwest of the central basin (Figure 26-2), because these oils seem to have migrated farthest from source beds. We show that these oils, which are produced from reservoirs more than 125 mi (200 km) from the basin's depocenter, were derived from Devonian source rocks in the deep basin. We then use quantitative models of the basin's paleohydrology to INTRODUCTION investigate the past subsurface conditions that drove the migration. We conclude that long-range migration The distribution of petroleum production from the was not related to processes occurring as the basin Illinois basin extends considerably beyond the area subsided and infilled. -
Geology of the Devonian Marcellus Shale—Valley and Ridge Province
Geology of the Devonian Marcellus Shale—Valley and Ridge Province, Virginia and West Virginia— A Field Trip Guidebook for the American Association of Petroleum Geologists Eastern Section Meeting, September 28–29, 2011 Open-File Report 2012–1194 U.S. Department of the Interior U.S. Geological Survey Geology of the Devonian Marcellus Shale—Valley and Ridge Province, Virginia and West Virginia— A Field Trip Guidebook for the American Association of Petroleum Geologists Eastern Section Meeting, September 28–29, 2011 By Catherine B. Enomoto1, James L. Coleman, Jr.1, John T. Haynes2, Steven J. Whitmeyer2, Ronald R. McDowell3, J. Eric Lewis3, Tyler P. Spear3, and Christopher S. Swezey1 1U.S. Geological Survey, Reston, VA 20192 2 James Madison University, Harrisonburg, VA 22807 3 West Virginia Geological and Economic Survey, Morgantown, WV 26508 Open-File Report 2012–1194 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Ken Salazar, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. -
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 -
Preliminary Geological Feasibility Report
R. L. LANGENHEfM, JR. EGN 111 DEPT. GEOL. UNIV. ILLINOIS 234 N.H. B., 1301 W. GREEN ST. URBANA, ILLINOIS 61801 Geological-Geotechnical Studies for Siting the Superconducting Super Collider in Illinois Preliminary Geological Feasibility Report J. P. Kempton, R.C. Vaiden, D.R. Kolata P.B. DuMontelle, M.M. Killey and R.A. Bauer Maquoketa Group Galena-Platteville Groups Illinois Department of Energy and Natural Resources ENVIRONMENTAL GEOLOGY NOTES 111 STATE GEOLOGICAL SURVEY DIVISION 1985 Geological-Geotechnical Studies for Siting the Superconducting Super Collider in Illinois Preliminary Geological Feasibility Report J.P. Kempton, R.C. Vaiden, D.R. Kolata P.B. DuMontelle, M.M. Killey and R.A. Bauer ILLINOIS STATE GEOLOGICAL SURVEY Morris W. Leighton, Chief Natural Resources Building 615 East Peabody Drive Champaign, Illinois 61820 ENVIRONMENTAL GEOLOGY NOTES 111 1985 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/geologicalgeotec1 1 1 kemp 1 INTRODUCTION 1 Superconducting Super Collider 1 Proposed Site in Illinois 2 Geologic and Hydrogeologic Factors 3 REGIONAL GEOLOGIC SETTING 5 Sources of Data 5 Geologic Framework 6 GEOLOGIC FRAMEWORK OF THE ILLINOIS SITE 11 General 1 Bedrock 12 Cambrian System o Ordovician System o Silurian System o Pennsylvanian System Bedrock Cross Sections 18 Bedrock Topography 19 Glacial Drift and Surficial Deposits 21 Drift Thickness o Classification, Distribution, and Description of the Drift o Banner Formation o Glasford Formation -
Bedrock Geology of Dixon West Quadrangle
STATEMAP Dixon West-BG Bedrock Geology of Dixon West Quadrangle Lee County, Illinois Dennis R. Kolata 2013 Prairie Research Institute ILLINOIS STATE GEOLOGICAL SURVEY 615 East Peabody Drive Champaign, Illinois 61820-6964 (217) 244-2414 http://www.isgs.illinois.edu © 2013 University of Illinois Board of Trustees. All rights reserved. For permission information, contact the Illinois State Geological Survey. INTRODUCTION STRATIGRAPHY The Dixon West Quadrangle is situated in northwestern Lee Bedrock in the Dixon West Quadrangle consists largely of County, Illinois. It encompasses the western parts of the city Ordovician dolomite and shale and a small area of Silurian of Dixon, which is the largest town in the county. Most of the dolomite in the southwestern part of the quadrangle. It has land is used for agricultural purposes but a moderate amount been standard practice of the ISGS during the past few of residential and commercial developments are present. decades to follow the Ordovician classification and nomen- clature proposed by Templeton and Willman (1963). Their The quadrangle lies in the Rock River Hill Country of the stratigraphy was followed in large part by Willman and Ko- Central Lowlands Province. The topography formed primar- lata (1978) who made minor revisions to some members and ily by deposition of glacial sediments (clay, silt, sand, and documented the presence of nine widespread K-bentonite gravel) in a till plain which was subsequently dissected by beds. These stratigraphic investigations have shown that the erosional processes of the Rock River and its tributaries. Upper Ordovician carbonate succession consists of distinc- Bedrock in the Dixon West Quadrangle is largely concealed tive rock units that can be traced over wide areas of the beneath the till plain except for local exposures along the riv- Midcontinent U.S. -
Geologic and Geochemical Studies of the New Albany Shale Group (Devonian-Mississippian) in Illinois
557 3M SuMr IL6of 1980-2 Final Report Geologic and Geochemical Studies of the New Albany Shale Group (Devonian-Mississippian) in Illinois R. E. Bergstrom and N. F. ShimP/ Principal Invistigators Robert M. Cluff, Project Coordinator Illinois State Geological Survey Open File Series 1980-2 June 30, 1980 Illinois State Geological Survey Urbana, IL 61801 Prepared for U.S. Department of Energy Morgantown Energy Technology Center Morgantown, WV 2 6505 Contract: U.S. Department of Energy DE-AC21-76ET12142 , Note to readers: Printouts of the data contained on the computer file and copies of the structure map mentioned in this report can be obtained from the Illinois State Geological Survey upon written request, This report was prepared as an account of work partially sponsored by the U.S. Government. Neither the United States nor the United States Depart- ment of Energy, nor any of their employees , contractors, subcontractors or employees makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. '^'NOIS STATE QEOLOQICAL SURVEY 3 305 Final Report Geologic and Geochemical Studies of the New Albany Shale Group (Devonian-Mississippian) in Illinois R. E. Bergstrom and N. F. Shimp, Principal Invistigators Robert M. Cluff, Project Coordinator Illinois State Geological Survey Open File Series 1980-2 SEP 1 1 1996 |L uluu ourWtY June 30, 1980 Illinois State Geological Survey Urbana, IL 61801 Prepared for U.S. Department of Energy Morgantown Energy Technology Center Morgantown, WV 2 6505 Contract: U.S. -
Mineral Resources of the Illinois Basin in the Context of Basin Evolution
Mineral Resources of the Illinois Basin in the Context of Basin Evolution St. Louis, Missouri, January 22-23,1992 Program and Abstracts Edited by Martin B. Goldhaber and J. James Eidel U.S. Geological Survey Open-File Report 92-1 This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey, Illinois State Geological Survey, Kentucky Geological Survey, Missouri Division of Geology and Land Survey, and Indiana Geological Survey standards. PREFACE The mineral resources of the U.S. midcontinent were instrumental to the development of the U.S. economy. Mineral resources are an important and essential component of the current economy and will continue to play a vital role in the future. Mineral resources provide essential raw materials for the goods consumed by industry and the public. To assess the availability of mineral resources and contribute to the abib'ty to locate and define mineral resources, the U.S. Geological Survey (USGS) has undertaken two programs in cooperation with the State Geological Surveys in the midcontinent region. In 1975, under the Conterminous U.S. Mineral Assessment Program (CUSMAP) work began on the Rolla 1° X 2° Quadrangle at a scale of 1:250,000 and was continued in the adjacent Springfield, Harrison, Joplin, and Paducah quadrangles across southern Missouri, Kansas, Illinois, Arkansas, and Oklahoma. Public meetings were held in 1981 to present results from the Rolla CUSMAP and in 1985 for the Springfield CUSMAP. In 1984, the Midcontinent Strategic and Critical Minerals Project (SCMP) was initiated by the USGS and the State Geological Surveys of 16 states to map and compile data at 1:1,000,000 scale and conduct related topical studies for the area from latitude 36° to 46° N. -
A Deposit Model for Mississippi Valley-Type Lead-Zinc Ores
A Deposit Model for Mississippi Valley-Type Lead-Zinc Ores Chapter A of Mineral Deposit Models for Resource Assessment 2 cm Sample of spheroidal sphalerite with dendritic sphalerite, galena, and iron sulfides (pyrite plus marcasite) from the Pomorzany mine. Note the “up direction” is indicated by “snow-on-the-roof” texture of galena and Scientificsphalerite Investigations alnong colloform Report layers of2010–5070–A light-colored spahlerite. Hydrothermal sulfide clasts in the left center of the sample are encrusted by sphalerire and iron sulfides. Size of sample is 20x13 cm. Photo by David Leach. U.S. Department of the Interior U.S. Geological Survey COVER: Sample of spheroidal sphalerite with dendritic sphalerite, galena, and iron sulfides (pyrite plus mar- casite) from Pomorzany mine. Note the “up direction” is indicated by “snow-on-the-roof” texture of galena and sphalerite along colloform layers of light-colored sphalerite. Hydrothermal sulfide clasts in the left center of the sample are encrusted by sphalerite and iron sulfides. Size of sample is 20x13 centimeters. (Photograph by David L. Leach, U.S. Geological Survey.) A Deposit Model for Mississippi Valley- Type Lead-Zinc Ores By David L. Leach, Ryan D. Taylor, David L. Fey, Sharon F. Diehl, and Richard W. Saltus Chapter A of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–A U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. -
Appendix 1. State Geologic Maps Bibliography
18 The State Geologic Map Compilation (SGMC) Geodatabase of the Conterminous United States Appendix 1. State Geologic Maps Bibliography The citations presented here are for the paper versions of the State geologic maps with a U.S. Geological Survey (USGS) National Geologic Map Database (NGMDB) URL link provided for convenience. The sources for all data in the State Geologic Map Compilation (SGMC) are the original USGS Preliminary Integrated Geologic Map Databases (PIGMD) unless otherwise noted. Please see the PIGMD citation provided for more detailed geologic map source information. Alabama (AL)—Scale 1:250,000 Osbourne, W.E., Szabo, M.W., Neathery, T.L., and Copeland, C.W., Jr., 1988, Geologic map of Alabama—Northeast sheet: Geological Survey of Alabama Special Map 220, scale 1:250,000. Szabo, M.W., and Copeland, C.W., Jr., 1988, Geologic map of Alabama—Southeast sheet: Geological Survey of Alabama Special Map 220, scale 1:250,000. Szabo, M.W., and Copeland, C.W., Jr., 1988, Geologic map of Alabama—Southwest sheet: Geological Survey of Alabama Special Map 220, scale 1:250,000. Szabo, M.W., Osbourne, W.E., and Copeland, C.W., Jr., 1988, Geologic map of Alabama—Northwest sheet: Geological Survey of Alabama Special Map 220, scale 1:250,000. NGMDB—Available at https://ngmdb.usgs.gov/Prodesc/proddesc_55859.htm. PIGMD—Available at https://pubs.usgs.gov/of/2005/1323/#AL. Arizona (AZ)—scale 1:1,000,000 Richard, S.M., Reynolds, S.J., Spencer, J.E., and Pearthree, P.A., 2000, Geologic map of Arizona: Arizona Geological Survey Map 35, 1 sheet, scale 1:1,000,000. -
Memorial to Harold Bowen Willman 1901-1984 JACK A
Memorial to Harold Bowen Willman 1901-1984 JACK A. SIMON and ELWOOD ATHERTON Illinois State Geological Survey, Champaign, Illinois 61820 Harold Bowen (“Bo”) Willman, died on July 4, 1984, in Urbana, Illinois, after a brief illness. He was an emi nent geologist performing basic and applied research for nearly 60 years in stratigraphy, structure, mineral deposits, and utilization of strata ranging from the Cambrian through the Pleistocene Systems primarily in Illinois and other midwestern states. He had a far- reaching impact on knowledge of the Ordovician, Silurian, Pennsylvanian, and Pleistocene Systems. Harold Bowen Willman, the son of Ernest Floyd and Gay Bowen Willman, was born July 30, 1901, in Newcastle, Indiana. He grew up and graduated from high school in Hartford City, Indiana. Bo went to the University of Illinois with an eye on courses in jour nalism, but he took a course in geology, and the expe rience changed his career. He received a B.A. in 1926, an M.A. in 1928, and a Ph.D. in 1931, all in geology. In the summer of 1924, he worked in British Columbia as a field assistant to Francis P. Shepard. In the summer of 1925, he worked for the Kentucky Geological Survey. In the summers of 1926 and 1927, he worked at the Illinois Geological Survey (ISGS), and was a graduate teaching assistant in geology at the University of Illinois. In 1928, Bo was appointed to the part-time staff at the Illinois State Geological Survey. Initially he worked with J. Marvin Weller in the Areal Geology and Paleontology Division during the summer, and with Gilbert H.