WVCCS Working Group Preliminary Report-Final (C1821197.DOC;1)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Fractured Shale Gas Potential in New York
FRACTURED SHALE GAS POTENTIAL IN NEW YORK David G. HILL and Tracy E. LOMBARDI TICORA Geosciences, Inc., Arvada, Colorado, USA John P. MARTIN New York State Energy Research and Development Authority, Albany, New York, USA ABSTRACT In 1821, a shallow well drilled in the Devonian age shale ushered in a new era for the United States when natural gas was produced, transported and sold to local establishments in the town of Fredonia, New York. Following this discovery, hundreds of shallow shale wells were drilled along the Lake Erie shoreline and eventually several shale gas fields were established southeastward from the lake in the late 1800’s. Since the mid 1900’s, approximately 100 wells have been drilled in New York to test the fractured shale potential of the Devonian and Silurian age shales. With so few wells drilled over the past century, the true potential of fractured shale reservoirs has not been thoroughly assessed, and there may be a substantial resource. While the resource for shale gas in New York is large, ranging from 163-313 trillion cubic feet (Tcf) and the history of production dates back over 180 years, it has not been a major contributor to natural gas production in New York. A review of the history and research conducted on the shales shows that the resource in New York is poorly understood and has not been adequately tested. Other shales such as the Silurian and Ordovician Utica Shale may also hold promise as new commercial shale gas reservoirs. Experience developing shale gas plays in the past 20 years has demonstrated that every shale play is unique. -
The Carboniferous Bowland Shale Gas Study: Geology and Resource Estimation
THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION The Carboniferous Bowland Shale gas study: geology and resource estimation i © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Disclaimer This report is for information only. It does not constitute legal, technical or professional advice. The Department of Energy and Climate Change does not accept any liability for any direct, indirect or consequential loss or damage of any nature, however caused, which may be sustained as a result of reliance upon the information contained in this report. All material is copyright. It may be produced in whole or in part subject to the inclusion of an acknowledgement of the source, but should not be included in any commercial usage or sale. Reproduction for purposes other than those indicated above requires the written permission of the Department of Energy and Climate Change. Suggested citation: Andrews, I.J. 2013. The Carboniferous Bowland Shale gas study: geology and resource estimation. British Geological Survey for Department of Energy and Climate Change, London, UK. Requests and enquiries should be addressed to: Toni Harvey Senior Geoscientist - UK Onshore Email: [email protected] ii © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Foreword This report has been produced under contract by the British Geological Survey (BGS). It is based on a recent analysis, together with published data and interpretations. Additional information is available at the Department of Energy and Climate Change (DECC) website. https://www.gov.uk/oil-and-gas-onshore-exploration-and-production. This includes licensing regulations, maps, monthly production figures, basic well data and where to view and purchase data. -
A2 and B2: Upper Devonian Kellwasser Extinction Events in New York and Pennsylvania: Offshore to Onshore Transect Across the F
A2 AND B2: UPPER DEVONIAN KELLWASSER EXTINCTION EVENTS IN NEW YORK AND PENNSYLVANIA: OFFSHORE TO ONSHORE TRANSECT ACROSS THE FRASNIAN-FAMENNIAN BOUNDARY ON THE EASTERN MARGIN OF THE APPALACHIAN BASIN ANDREW M. BUSH AND J. ANDREW BEARD Geosciences & Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT 06269 GORDON BAIRD Department of Geosciences, SUNY Fredonia, Fredonia, NY 14063 D. JEFFREY OVER Department of Geological Sciences, SUNY Geneseo, Geneseo, NY 14454 with contributions by KATHERINE TUSKES Department of Geological Sciences, Atmospheric, Ocean, and Earth Science, George Mason University, Manassas, VA 20110 SARAH K. BRISSON AND JALEIGH Q. PIER Geosciences & Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT 06269 INTRODUCTION Earth-system perturbations caused a series of mass extinction events during the Devonian Period, including the Taghanic event in the Givetian, the Lower and Upper Kellwasser events in the Frasnian, and the Hangenberg event in the Famennian (House, 2002; Bambach, 2006). These extinctions occurred against the backdrop of orbitally forced sea-level fluctuations, the Acadian Orogeny (Averbuch et al., 2005), the expansion of plants and animals on land (Algeo et al., 1995), and ecological changes in the marine biosphere (Signor and Brett, 1984; Bambach, 1999). The Frasnian-Famennian boundary in particular represents a significant global crisis, considered one of the “big five” mass extinctions (Raup and Sepkoski, 1982) that led to the demise of the widespread and diverse Devonian -
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, By GEORGE V. COHEE, ROBERT G. BATES, and WILNA B. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1294-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 35 cents (paper cover) CONTENTS Listing of nomenclatural changes- --- ----- - - ---- -- -- -- ------ --- Ortega Quartzite and the Big Rock and Jawbone Conglomerate Members of the Kiawa Mountain Formation, Tusas Mountains, New Mexico, by Fred Barker---------------------------------------------------- Reasons for abandonment of the Portage Group, by Wallace de Witt, Jr-- Tlevak Basalt, west coast of Prince of Wales Island, southeastern Alaska, by G. Donald Eberlein and Michael Churkin, Jr Formations of the Bisbee Group, Empire Mountains quadrangle, Pima County, Arizona, by Tommy L. Finnell---------------------------- Glance Conglomerate- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - Willow Canyon Formation ....................................... Apache Canyon Formation-- ................................... Shellenberger Canyon Formation- - --__----- ---- -- -- -- ----------- Turney Ranch Formation---- ------- ------ -- -- -- ---- ------ ----- Age--_------------------------------------------------------- Pantano Formation, by Tommy L. Finnell----------_----------------- -
Dinantian Carbonate Development and Related Prospectivity of the Onshore Northern Netherlands
Dinantian carbonate development and related prospectivity of the onshore Northern Netherlands Nynke Hoornveld, 2013 Author: Nynke Hoornveld Supervisors: Bastiaan Jaarsma, EBN Utrecht Prof. Dr. Jan de Jager, VU University Amsterdam Master Thesis: Solid Earth, (450199 and 450149) 39 ECTS. VU University Amsterdam 01-06-2013 Dinantian carbonate development and related prospectivity of the onshore Northern Netherlands Nynke Hoornveld, 2013 Contents Contents……………………………………………………………………………………………………………………………………………..2 Abstract…………………………………………………………………………………………….………………………………………………..3 Introduction…………………………………………………………………………………………………………….…………………….……4 Geological History of the Netherlands relating to Dinantian development…………………………..……………..7 Tectonic history…………………………………………………………………………………………………………………………..9 Stratigraphy of the Carboniferous…………………………………………………………………………………………….16 Stratigraphic Nomenclature of the Netherlands……………………………………………………………….………23 Methods……………………………………………………………………………………………………………………………………….…..26 Seismic interpretation…………………………………………………………………………………………………………….…27 Time-depth conversion…………………………………………………………………………………………………….……...35 Well correlation……………………………………………………………………………………………………………………..…38 Carbonate production, precipitation and geometries, with a focus on the Dinantian……….………40 Results………………………………………………………………………………………………………………………………….…………..57 Well information, evaluation and reservoir development………………………………………………………..58 Geometry of the Dinantian carbonate build-ups in the Dutch Northern onshore…………..……….75 The geological history -
Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia
Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia By: Jonathan Prevatte August 2020 Director of Thesis: Donald W. Neal Major Department: Geological Sciences Petroleum is one of the main sources for energy production in the US and is therefore important for the continuation of economic growth. Future development of petroleum resources in the US to meet supply demands is equally important. Understanding the controls on petroleum production will help in determining where and how to development these resources for maximum production. West Virginia is home to many gas fields and is underlain by one of the more prominent gas producing shales, the Marcellus Shale. The Clendenin Gas Field in Kanawha County is one of the historical gas producing areas found in West Virginia. This assessment is focused on the Devonian strata throughout the field including the Marcellus Shale. Using available geophysical logs, production data, and historic well records obtained from the West Virginia Geologic and Economic Survey (WVGES), cross-sections, isopach maps, and structure contour maps were created to give a visual representation of the subsurface geology across the field. Construction of the cross-sections and maps in conjunction with production and well record data aided in the identification of controls influencing production throughout the field. Applying the findings of this assessment to future production may reduce costs and improve yields of future petroleum wells. Results of this study indicate several options should be considered when planning for future production wells within the field. Target areas include the areas to the east of the field where formations tend to thicken. -
Xsec A-A Sht1of2 Layout FINAL V
U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 3425 U.S. GEOLOGICAL SURVEY (SHEET 1 OF 2) Explanatory pamphlet accompanies map A Ontario Allegheny Lowlands Plateau province province SEVERNE WATKINS-BEAVER LODI POINT FIRTREE DAMS ALPINE VAN ETTEN ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE GLENORA SYNCLINE UNNAMED COHOCTON CORBETT POINT ENFIELD CAYUTA SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE Bend in section Bend in section Bend in section New York W SE Oatka Genesee NW SE Canisteo NW SW Pennsylvania Black Creek River Canaseraga River Tuscarora Creek Creek Creek FEET MILES 0 10 20 30 40 50 60 70 80 90 3,000 1 2 3 4 5 6 William Duchscherer, Jr. E.F. Blair and Associates NYS Natural Gas Company E.F. Blair and Associates Bowdoin Storage Service Inc. NYS Natural Gas Company No. 1 J. Klotzbach No. 1 L. Tyler No. 1 Albert McClurg No. 1 Arthur N. Kennedy No. 1 Hubbard No. 1 Robert Olin API No. 31-037-05117 API No. 31-037-04593 API No. 31-051-04552 API No. 31-051-04630 API No. 31-101-21496 API No. 31-101-03924 Genesee Co., New York Genesee Co., New York Livingston Co., New York Livingston Co., New York Steuben Co., New York Steuben Co., New York Perrysburg Formation Dunkirk Dunkirk Shale Shale 2,000 Member Wiscoy Sandstone Member Java Perrysburg West River Shale, Nunda Wiscoy Sandstone Member Formation Formation Genundewa Sandstone Member unnamed Pipe Creek 0 Pipe Creek shale member Limestone, Penn Member Shale Member Shale Member Perrysburg Yan Shale, and rmation Formation 0 Dun West River Shale, Java Fo kirk -
WV Generalized Stratigraphic Column/Chart
Generalized Stratigraphic Chart for West Virginia Series/ Drillers’ Era System Stage Western WV Eastern WV Terminology CENOZOIC Paleogene Eocene Igneous Intrusives MESOZOIC Jurassic Igneous Intrusives PERMIAN Dunkard Group Carroll, Minshall, Murphy, Moundsville, Upper Monongahela Fm. 1st Cow Run, Little Conemaugh Group Dunkard, Big Dunkard Burning Springs, Middle Allegheny Fm. 2nd Cow Run, Kanawha Fm. Gas Sands, Horseneck (Subsystem) New River Fm. Pottsville PENNSYLVANIAN Lower Pocahontas Fm. Group Salt Sands Bluestone Fm. Pride, Ravencliff, Avis, Princeton Ss. Mauch Chunk Maxton, Little Lime, Upper Hinton Fm. Group Pencil Cave, Blue Monday Bluefield Fm. CARBONIFEROUS Greenbrier Group Big Lime, Keener, Middle Big Injun (Subsystem) Maccrady Fm. (south) MISSISSIPPIAN Lower Big Injun, Squaw, Sunbury Sh. Price Fm. Weir, Coffee (Sunbury) Sh. Berea Ss. Cleveland Sh. Gantz, 50’, 30’, Ohio Sh. Chagrin Sh. Hampshire Group Huron Sh. Gordon Stray, Gordon, Hanover Sh. bed 4th, 5th, Bayard, Java Fm. Pipe Creek Sh. bed Greenland Foreknobs Fm. Elizabeth, Warren, Upper West Falls Fm. Angola Sh. Gap Group Scherr Fm. Speechley, Balltown, Rhinestreet Sh. Bradford, Riley, Cashaqua Sh. Sonyea Fm. Middlesex Sh. Benson, Alexander, Elk, Haverty, Genesee Fm./ West River Sh. Brallier Fm. Geneseo Sh./Burket Sh. Fox, Sycamore Harrell Sh. Harrell Sh. DEVONIAN Tully Ls. Millboro Sh. Hamilton Group Mahantango Fm. Mahantango Fm. Marcellus Sh. Marcellus Sh. Middle Tioga ash beds Tioga ash beds Huntersville Chert Needmore Sh. Onondaga Ls. Oriskany Ss. “Corniferous” Lower (west only) Helderberg Group Bass Islands Fm. Big Mountain Sh. Clifton Forge Ss. Keyser Fm. PALEOZOIC Lower Keyser Mbr. PHANEROZOIC Salina Fm. Tonoloway Fm. Newburg Wills Creek Fm. Upper Bloomsburg Williamsport Fm. Fm. -
Winchester Stone by Dr John Parker (PDF)
Winchester Stone by John Parker ©2016 Dr John Parker studied geology at Birmingham and Cambridge universities. He is a Fellow of the Geological Society of London. For over 30 years he worked as an exploration geologist for Shell around the world. He has lived in Winchester since 1987. On retirement he trained to be a Cathedral guide. The Building of Winchester Cathedral – model in the Musée de la Tapisserie, Bayeux 1 Contents Introduction page 3 Geological background 5 Summary of the stratigraphic succession 8 Building in Winchester Romano-British and Anglo-Saxon periods 11 Early medieval period (1066-1350) 12 Later medieval period (1350-1525) 18 16th to 18th century 23 19th to 21st century 24 Principal stone types 28 Chalk, clunch and flint 29 Oolite 30 Quarr 31 Caen 33 Purbeck 34 Beer 35 Upper Greensand 36 Portland 38 Other stones 40 Weldon 40 Chilmark 41 Doulting 41 French limestones 42 Coade Stone 42 Decorative stones, paving and monuments 43 Tournai Marble 43 Ledger stones and paving 44 Alabaster 45 Jerusalem stone 45 Choice of stone 46 Quarries 47 A personal postscript 48 Bibliography and References 50 ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Photographs and diagrams are by the author, unless otherwise indicated 2 Introduction Winchester lies in an area virtually devoid of building stone. The city is on the southern edge of the South Downs, a pronounced upland area extending from Salisbury Plain in the west to Beachy Head in the east (Figs. 1 & 2). The bedrock of the Downs is the Upper Cretaceous Chalk (Fig. 3), a soft friable limestone unsuited for major building work, despite forming impressive cliffs along the Sussex coast to the east of Brighton. -
Eastern Section American Association of Petroleum Geologists 46Th Annual Meeting Morgantown, West Virginia September 24-27, 2017
Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Meeting Sponsors We appreciate your support! Marcellus Level Meeting Sponsors Utica Level Rogersville Level We appreciate your support! Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Cover photo used with permission from Jacob Everhart, Canary, LLC Contents Welcome………………………………………………………………………………………………………………………………………1 2017 Meeting Organizing Committee……………………………………………………………………………….1 Eastern Section AAPG Officers………………………………………………………………………………………….2 Appalachian Geological Society Officers……………………………………………………………………………2 General Information…………………………………………………………………………………………………………………….3 Registration Hours……………………………………………………………………………………………………………3 Parking………………………………………………………………………………………………………………………….….3 Maps………………………………………………………………………………………………………………………………..3 Exhibits……………………………………………………………………………………………………………………….……3 Presenters and Judges Room……………………………………………………………………………………..….…3 Presenters, Judges and Session Chairs Breakfast and Information……………………………………3 -
WVCCS Working Group Final Report-June 30, 2011 (C2091773
i This page has been intentionally left blank. TABLE OF CONTENTS Summary of Terminology, Abbreviations, and Acronyms ……………………….… i List of Working Group Members ……………………………………………….…… iii I. Executive Summary ………………………………………………..…………… 1 A. Background………………………………………………………………… 1 B. Organization of the Final Report…………………………………….…… 2 C. Feasibility Subcommittee …………………………………………..…….. 2 D. Geology & Technical Committee ……………………………………..….. 4 E. Legal Subcommittee …………………………………………………..….. 6 F. Summary……………………………………………………………..…… 8 II. Details of the Working Group ……………………………………...……..…… 8 A. Meetings …………………………………………........ ………………… 8 B. Resources …………………………………………………………………. 8 III. Statutes of the Regulation of Greenhouse Gases …………………………… 9 IV. Subcommittee Reports ……………………………………………………..… 12 A. Feasibility Subcommittee Report…………………………………………. 12 Question 1: What factors need to be considered in determining if CCS is feasible and beneficial for West Virginia? ……………………… 28 Question 2: What factors need to be addressed to be able to be addressed prior to reaching a decision regarding the feasibility of encouraging CCS in West Virginia? ………………………………..……. 38 Question 3: What are the technical issues (both engineering and geological) that must be addressed to ensure the efficacy of CCS in West Virginia? ……………………………………………………………. 46 B. Geology & Technology Report …………………………………………… 46 Question 4: What legal and liability issues need to be decided before CCS can be pursued in West Virginia? ……………….…………………. 99 C. Legal Subcommittee Report ……………………………………………… -
Figure 2 (Pdf)
South North West East West East West East West East Eastern Kentucky Central West Virginia Eastern and Central Ohio Western and Central Pennsylvania Western and Central New York Age Stratigraphy from: Repetski and others (2008) Stratigraphy from: Ryder and others (2008, 2009) Stratigraphy from: Ryder and others (2008, 2009, 2010) Stratigraphy from: Berg and others (1983); Ryder and others (2010) Stratigraphy from: Repetski and others (2008) Era System Series (Ma) Valley Valley Rome Trough Rome Trough Rome Trough and Ridge Bedford Shale and Ridge Cleveland Member Venango Group Catskill Formation 359.2 Upper Devonian strata, undivided Ohio Shale Ohio Three Lick Bed Chagrin Shale equivalent rocks Chagrin Shale Bradford Group Foreknobs Formation Perrysburg Formation Shale Dunkirk Shale Member Huron Member of Ohio Shale Huron Member Elk Group Scherr Formation Upper Dunkirk Shale Java Formation Angola Shale Member Olentangy Shale (upper) Java Formation Java Formation Angola Shale Member West Falls West Falls Brallier Formation West Falls Angola Shale Member Formation Rhinestreet Shale Member Rhinestreet Shale Member of the Formation Rhinestreet Shale Member Formation Rhinestreet Shale Member Upper Devonian strata, undivided West Falls Formation 385.3 Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Tully Limestone Tully Limestone Tully Limestone Mahantango Formation Mahantango Formation Moscow, Ludlowville, and Skaneateles Shales, undivided Hamilton Olentangy Shale (lower)