Clay and Shale Resources of Ontario
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Technology Technical Report
Technology Technical Report HYDRAULIC FRACTURING IN THE STATE OF MICHIGAN ABOUT THIS REPORT This document is one of the seven technical reports com- pleted for the Hydraulic Fracturing in Michigan Integrated Assessment conducted by the University of Michigan. During the initial phase of the project, seven faculty-led and student-staffed teams focused on the following topics: Technology, Geology/ Hydrogeology, Environment/Ecology, Human Health, Policy/ Law, Economics, and Public Perceptions. These reports were prepared to provide a solid foundation of information on the topic for decision makers and stakeholders and to help inform the Integrated Assessment, which will focus on the analysis of policy options. The reports were informed by comments from (but do not necessarily reflect the views of) the Integrated Assessment Steering Committee, expert peer reviewers, and numerous public comments. Upon completion of the peer review process, final decisions regarding the content of the reports were deter- mined by the faculty authors in consultation with the peer review editor. These reports should not be characterized or cited as final products of the Integrated Assessment. The reports cover a broad range of topics related to hydraulic fracturing in Michigan. In some cases, the authors determined that a general discussion of oil and gas development is important to provide a framing for a more specific discussion of hydraulic fracturing. The reports address common hydraulic fracturing (HF) as meaning use of hydraulic fracturing methods regardless of well depth, fluid volume, or orientation of the well (whether vertical, directional, or horizontal). HF has been used in thousands of wells throughout Michigan over the past several decades. -
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 -
Undiscovered Oil and Gas Resources Underlying the US Portions of The
The eight continuous AUs (and associated basins) are as follows: Table 2. Summary of mean values of Great Lakes oil and National Assessment of Oil and Gas Fact Sheet 1. Pennsylvanian Saginaw Coal Bed Gas AU (Michigan Basin), gas resource allocations by lake. 2. [Devonian] Northwestern Ohio Shale AU (Appalachian Basin), [Compiled from table 1, which contains the full range of statistical 3. [Devonian] Marcellus Shale AU (Appalachian Basin), values] Undiscovered Oil and Gas Resources Underlying the 4. Devonian Antrim Continuous Gas AU (Michigan Basin), 5. Devonian Antrim Continuous Oil AU (Michigan Basin), Total undiscovered resources U.S. Portions of the Great Lakes, 2005 6. [Silurian] Clinton-Medina Transitional AU (Appalachian Basin), Oil Gas Natural gas 7. [Ordovician] Utica Shale Gas AU (Appalachian Basin), and (million (trillion liquids 8. Ordovician Collingwood Shale Gas AU (Michigan Basin). barrels), cubic feet), (million barrels), Of these eight continuous AUs, only the following four AUs were Lake mean mean mean Lake bathymetry (meters) 300 - 400 assessed quantitatively: [Silurian] Clinton-Medina Transitional AU, Devo- he U.S. Geological Survey recently completed Lake Erie 46.10 3.013 40.68 T 200 - 300 nian Antrim Continuous Gas AU, [Devonian] Marcellus Shale AU, and Lake Superior allocations of oil and gas resources underlying the U.S. por- 100 - 200 Allocation [Devonian] Northwestern Ohio Shale AU. The other four continuous AUs Lake Huron 141.02 0.797 42.49 area tions of the Great Lakes. These allocations were developed 0 - 100 lacked sufficient data to assess quantitatively. Lake Michigan 124.59 1.308 37.40 from the oil and gas assessments of the U.S. -
EMD Shale Gas and Liquids Committee Annual Report, FY 2014
EMD Shale Gas and Liquids Committee Annual Report, FY 2014 Neil S. Fishman, Chair March 30, 2014 Vice Chairs: Brian Cardott, (Vice Chair, Government), Oklahoma Geological Survey, Norman, OK Harris Cander (Vice Chair, Industry), BP, Houston, TX Sven Egenhoff, (Vice Chair, University), Colorado State University, Fort Collins, CO Advisory Committee (in alphabetical order): Kent Bowker, Bowker Petroleum, The Woodlands, TX Ken Chew, IHS (retired), Perthsire, Scotland Thomas Chidsey, Utah Geological Survey, Salt Lake City, UT Russell Dubiel, U.S. Geological Survey, Denver, CO Catherine Enomoto, U.S. Geological Survey, Reston, VA William Harrison, Western Michigan University, Kalamazoo, MI Ursula Hammes, Bureau of Economic Geology, Austin, TX Shu Jiang, University of Utah, Salt Lake City, UT Margaret Keller, U.S. Geological Survey, Menlo Park, CA Julie LeFever, North Dakota Geological Survey, Grand Forks, ND Peng Li, Arkansas Geological Survey, Little Rock, AR Jock McCracken, Egret Consulting, Calgary, AB Stephen Nordeng, North Dakota Geological Survey, Grand Forks, ND Rich Nyahay, New York Museum, Albany, NY Stephen Sonnenberg, Colorado School of Mines, Golden, CO Michael D. Vanden Berg, Utah Geological Survey, Salt Lake City, UT Rachel Walker, Countrymark Energy Resources, LLC, Indianapolis, IN INTRODUCTION It is a pleasure to present this Annual Report from the EMD Shale Gas and Liquids Committee. This report contains information about specific shales across the U.S., Canada, Europe, China, as well as SE Asia from which hydrocarbons are currently being produced or shales that are of interest for hydrocarbon exploitation. The inclusion in this report of shales from which any hydrocarbon is produced reflects the expanded mission of the EMD Shale Gas and Liquids Committee to serve as a single point of access to technical information on shales regardless of the hydrocarbons produced from them (e.g., gas, oil, condensate). -
Geology of Michigan and the Great Lakes
35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed. -
Collingwood Mb., Lindsay Fm., Stratigraphy and Oil Shale Potential
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
021-1570 Fnl Rpt 4 Feb 03 LLW Geotech Feas Study.Doc
Golder Associates Ltd. 2390 Argentia Road Mississauga, Ontario, Canada L5N 5Z7 Telephone: (905) 567-4444 Fax: (905) 567-6561 REPORT ON LLW GEOTECHNICAL FEASIBILITY STUDY WESTERN WASTE MANAGEMENT FACILITY BRUCE SITE TIVERTON, ONTARIO Submitted to: Municipality of Kincardine and Ontario Power Generation Nuclear Waste Management Division 700 University Avenue Toronto, Ontario M5G 1X6 DISTRIBUTION: 4 Copies - Municipality of Kincardine 4 Copies - Ontario Power Generation 2 Copies - Golder Associates Ltd. January 2003 021-1570 OFFICES ACROSS NORTH AMERICA, SOUTH AMERICA, EUROPE, AFRICA, ASIA AND AUSTRALIA January 2003 -i- 021-1570 SUMMARY This report presents the results of an assessment of the geotechnical feasibility of constructing a LLW permanent repository at OPG’s Western Waste Management Facility at the former Bruce Nuclear Power Development site near Tiverton, Ontario (the Bruce Site). The assessment was undertaken as part of activities associated with a Memorandum of Understanding between OPG and the Municipality of Kincardine and considered a number of generic LLW repository concepts previously developed by OPG, specifically: • three near surface concepts involving emplacement of LLW in structural concrete vaults located on ground surface (Covered Above Grade Concrete Vault), in a shallow trench at a depth of about 10 m to 15 m below ground surface (Shallow Concrete Vault) and in a deep trench at a depth of about 25 m below ground surface (Deep Concrete Vault); and • four Rock Cavern Vault concepts involving emplacement of LLW in unlined, mined caverns in the bedrock at a depth of about 50 m to 100 m below ground surface (Shallow Rock Cavern Vault) and at depths of about 200 m to 800 m below ground surface (Deep Rock Cavern Vault) in (i) a thick salt bed, (ii) a low permeability shale sequence, and (iii) a low permeability limestone sequence which were projected to underlie the Site. -
Geology and Resources of Some World Oil-Shale Deposits
Geology and Resources of Some World Oil-Shale Deposits Scientific Investigations Report 2005–5294 U.S. Department of the Interior U.S. Geological Survey Cover. Left: New Paraho Co. experimental oil shale retort in the Piceance Creek Basin a few miles west of Rifle, Colorado. Top right: Photo of large specimen of Green River oil shale interbedded with gray layers of volcanic tuff from the Mahogany zone in the Piceance Creek Basin, Colorado. This specimen is on display at the museum of the Geological Survey of Japan. Bottom right: Block diagram of the oil shale resources in the Mahogany zone in about 1,100 square miles in the eastern part of the Uinta Basin, Utah. The vertical scale is in thousands of barrels of in-place shale oil per acre and the horizontal scales are in UTM coordinates. Illustration published as figure 17 in U.S. Geological Survey Open-File Report 91-0285. Geology and Resources of Some World Oil-Shale Deposits By John R. Dyni Scientific Investigations Report 2005–5294 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Dirk Kempthorne, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 Posted onlline June 2006 Version 1.0 This publication is only available online at: World Wide Web: http://www.usgs.gov/sir/2006/5294 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. -
Shale Gas Opportunities in Southern Ontario – an Update
Shale Gas Opportunities in Southern Ontario – an Update Terry Carter, Ministry of Natural Resources, London, ON Lee Fortner, Ministry of Natural Resources, London, ON Catherine Béland-Otis, Ontario Geological Survey, Sudbury, ON 48th Annual OPI Conference and Trade Show Sarnia, Ontario Acknowledgements • Oil, Gas and Salt Resources Library • Staff of Petroleum Resources Centre, MNR • Tony Hamblin, GSC – Open File Report 5384 Regional Geological Setting and Shale Gas Plays Potential gas shales in Ontario Same plays as in NE U.S. and Quebec Best potential in: – U. Devonian Kettle Point Fm (Antrim shale equivalent) – M. Devonian Marcellus Formation – U. Ordovician Blue Mountain Formation and Collingwood shale (Utica equivalents) • Gas shows, no current production • Unexplored (only one shale gas exploratory well) • Large prospective areas Age Windsor-Essex London area Niagara Peninsula - Sunbury Pt ton Berea Lamb Bedford Upper Kettle Point Kettle Point Kettle Point Ipperwash Widder Hungry Hollow Hungry Hollow Arkona Hamilton Rockport Quarry Arkona Bell Hamilton Middle Marcellus Marcellus Dundee Dundee Dundee Devonian Lucas Lucas River River R. Detroit Detroit Detroit Detroit De Amherstburg Amherstburg t. Amherstburg Bois Blanc Bois Blanc Bois Blanc Lower Oriskany Bass Islands Bass Islands Bass Islands - Bertie Subsurface G unit G unit G unit F unit F unit F unit E unit E unit E unit D unit C unit C unit C unit Upper Salina Salina Salina B unit B B Paleozoic A-2 unit A-2 unit A-2 unit A unit A unit A-1 unit A-1 unit A-1 unit Guelph Guelph Guelph Eramosa Eramosa Eramosa Stratigraphic Goat Island Goat Island Gasport Gasport Wiarton Decew Rochester Middle Amabel Amabel Lockport Chart Silurian Rochester Irondequoit Reynales Reynales Fossil Hill Thorold Cabot Head Grimsby Cabot Head Manitoulin Man. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. XXI, NO. 10, pp. 219-229 JULY 3, 1967 ORDOVICIAN AND SILURIAN STRATA FROM WELL CORE IN SCHOOLCRAFT COUNTY, MICHIGAN BY GEORGE M. EHLERS, ROBERT V. KESLING, and ARTHUR E. SLAUGHTER MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: LEWISB. KELLUM 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. VOLS.11-XX. Parts of volumes may be obtained if available. VOLUMEXXI 1. Fossils from the Seymour Formation of Knox and Baylor Counties, Texas, and their bearing on the Late Kansan Climate of that Region, by Claude W. Hibbard and Walter W. Dalquest, Pages 1-66, with 5 plates and 8 figures. 2. Planalveolitella, a new genus of Devonian Tabulate Corals, with a rede- scription of Planalveolites faughti (Edwards and Haime), by Erwin C. Stumm, Pages 67-72, with 1 plate. 3. Neopalaeaster enigmeticus, New Starfish from Upper Mississippian Paint Creek Formation in Illinois, by Robert V. Kesling, Pages 73-85, with plates and 3 figures. 4. Tabulate Corals of the Silica Shale (Middle Devonian) of Northwestern Ohio and Southeastern Michigan, by Erwin C. -
Geophysical and Geological Analysis of the Collingwood Member of the Trenton Formation
Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Dissertations, Master's Theses and Master's Reports - Open Reports 2012 Geophysical and geological analysis of the Collingwood Member of the Trenton Formation Ryan M. Banas Michigan Technological University Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geophysics and Seismology Commons Copyright 2012 Ryan M. Banas Recommended Citation Banas, Ryan M., "Geophysical and geological analysis of the Collingwood Member of the Trenton Formation", Master's Thesis, Michigan Technological University, 2012. https://doi.org/10.37099/mtu.dc.etds/312 Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Geophysics and Seismology Commons A GEOPHYSICAL AND GEOLOGICAL ANALYSIS OF THE COLLINGWOOD MEMBER OF THE TRENTON FORMATION By Ryan M. Banas A THESIS Submitted in partial fulfilment of the requirements for the degree of MASTER OF SCIENCE (Geophysics) MICHIGAN TECHNOLOGICAL UNVIERSITY 2011 © 2011 Ryan M. Banas This thesis, “A Geophysical and Geological Analysis of the Collingwood Member of the Trenton Formation,” is hereby approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE IN GEOPHYSICS. Department of Geological and Mining Engineering and Sciences Signatures: Thesis Advisor ______________________________ Wayne D. Pennington Department Chair ______________________________ Wayne D. Pennington Date ______________________________ TABLE OF CONTENTS -
Clay, Shale Deposits
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”).