Qualitative and Quantitative Analysis of Carbonate Waters in the Peters Mountain Region of Monroe County, WV
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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. -
A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin
DOE/NETL-2011/1478 A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin U.S. DEPARTMENT OF ENERGY DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed 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 upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. ACKNOWLEDGMENTS The authors greatly thank Daniel J. Soeder (U.S. Department of Energy) who kindly reviewed the manuscript. His criticisms, suggestions, and support significantly improved the content, and we are deeply grateful. Cover. Top left: The Barnett Shale exposed on the Llano uplift near San Saba, Texas. Top right: The Marcellus Shale exposed in the Valley and Ridge Province near Keyser, West Virginia. Photographs by Kathy R. Bruner, U.S. Department of Energy (USDOE), National Energy Technology Laboratory (NETL). Bottom: Horizontal Marcellus Shale well in Greene County, Pennsylvania producing gas at 10 million cubic feet per day at about 3,000 pounds per square inch. -
Figure 3A. Major Geologic Formations in West Virginia. Allegheney And
82° 81° 80° 79° 78° EXPLANATION West Virginia county boundaries A West Virginia Geology by map unit Quaternary Modern Reservoirs Qal Alluvium Permian or Pennsylvanian Period LTP d Dunkard Group LTP c Conemaugh Group LTP m Monongahela Group 0 25 50 MILES LTP a Allegheny Formation PENNSYLVANIA LTP pv Pottsville Group 0 25 50 KILOMETERS LTP k Kanawha Formation 40° LTP nr New River Formation LTP p Pocahontas Formation Mississippian Period Mmc Mauch Chunk Group Mbp Bluestone and Princeton Formations Ce Obrr Omc Mh Hinton Formation Obps Dmn Bluefield Formation Dbh Otbr Mbf MARYLAND LTP pv Osp Mg Greenbrier Group Smc Axis of Obs Mmp Maccrady and Pocono, undivided Burning Springs LTP a Mmc St Ce Mmcc Maccrady Formation anticline LTP d Om Dh Cwy Mp Pocono Group Qal Dhs Ch Devonian Period Mp Dohl LTP c Dmu Middle and Upper Devonian, undivided Obps Cw Dhs Hampshire Formation LTP m Dmn OHIO Ct Dch Chemung Group Omc Obs Dch Dbh Dbh Brailler and Harrell, undivided Stw Cwy LTP pv Ca Db Brallier Formation Obrr Cc 39° CPCc Dh Harrell Shale St Dmb Millboro Shale Mmc Dhs Dmt Mahantango Formation Do LTP d Ojo Dm Marcellus Formation Dmn Onondaga Group Om Lower Devonian, undivided LTP k Dhl Dohl Do Oriskany Sandstone Dmt Ot Dhl Helderberg Group LTP m VIRGINIA Qal Obr Silurian Period Dch Smc Om Stw Tonoloway, Wills Creek, and Williamsport Formations LTP c Dmb Sct Lower Silurian, undivided LTP a Smc McKenzie Formation and Clinton Group Dhl Stw Ojo Mbf Db St Tuscarora Sandstone Ordovician Period Ojo Juniata and Oswego Formations Dohl Mg Om Martinsburg Formation LTP nr Otbr Ordovician--Trenton and Black River, undivided 38° Mmcc Ot Trenton Group LTP k WEST VIRGINIA Obr Black River Group Omc Ordovician, middle calcareous units Mp Db Osp St. -
Structural Geology of the Transylvania Fault Zone in Bedford County, Pennsylvania
University of Kentucky UKnowledge University of Kentucky Master's Theses Graduate School 2009 STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Elizabeth Lauren Dodson University of Kentucky, [email protected] Right click to open a feedback form in a new tab to let us know how this document benefits ou.y Recommended Citation Dodson, Elizabeth Lauren, "STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA" (2009). University of Kentucky Master's Theses. 621. https://uknowledge.uky.edu/gradschool_theses/621 This Thesis is brought to you for free and open access by the Graduate School at UKnowledge. It has been accepted for inclusion in University of Kentucky Master's Theses by an authorized administrator of UKnowledge. For more information, please contact [email protected]. ABSTRACT OF THESIS STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Transverse zones cross strike of thrust-belt structures as large-scale alignments of cross-strike structures. The Transylvania fault zone is a set of discontinuous right-lateral transverse faults striking at about 270º across Appalachian thrust-belt structures along 40º N latitude in Pennsylvania. Near Everett, Pennsylvania, the Breezewood fault terminates with the Ashcom thrust fault. The Everett Gap fault terminates westward with the Hartley thrust fault. Farther west, the Bedford fault extends westward to terminate against the Wills Mountain thrust fault. The rocks, deformed during the Alleghanian orogeny, are semi-independently deformed on opposite sides of the transverse fault, indicating fault movement during folding and thrusting. Palinspastic restorations of cross sections on either side of the fault zone are used to compare transverse fault displacement. -
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EVALUATION OF POTENTIAL STACKED SHALE-GAS RESERVOIRS ACROSS NORTHERN AND NORTH-CENTRAL WEST VIRGINIA ABSTRACT Jessica Pierson Moore1, Susan E. Pool1, Philip A. Dinterman1, J. Eric Lewis1, Ray Boswell2 Three shale-gas units underlying northern and north-central West Virginia create opportunity for one horizontal well pad to produce from multiple zones. The Upper Ordovician Utica/Point Pleasant, Middle Devonian Marcellus, and Upper Devonian Burket/Geneseo 1 West Virginia Geological & Economic Survey, 2 U.S. DOE National Energy Technology Laboratory construction of fairway maps for each play. Current drilling activity focuses on the Marcellus, with more than 1,000 horizontal completions reported through mid-2015. Across northern West Virginia, the Marcellus is 40 to 60 ft. thick with a depth range between 5,000 and 8,000 ft. Total Organic Carbon (TOC) REGIONAL GEOLOGY is generally 10% or greater. Quartz content is relatively high (~60%) and clay content is low (~30%). Reservoir pressure estimates STRUCTURAL CROSS-SECTION FROM HARRISON CO., OHIO TO HARDY CO., WEST VIRGINIA range from 0.3 to 0.7 psi/ft and generally increase to the north. Volumetric assessment of the Marcellus in this area yields preliminary NW SE 81° 80° 79° 78° 1 2 3 4 5 original gas-in-place estimates of 9 to 24 Bcf/mi2. OH WV WV WV WV Pennsylvania Figure 2.—Location of seismic sections, wells, and major basement Harrison Co. Marshall Co. Marion Co. Preston Co. Hardy Co. 34-067-20103 47-051-00539 47-049-00244 47-077-00119 47-031-00021 UTICA SHALE PLAY GR 41 miles GR 36 miles GR 27 miles GR 32 miles GR Westmoreland The Burket /Geneseo interval is approximately 15 to 40 ft thick across the fairway. -
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. -
Proterozoic Paleozoic Cambrian Ordovician Silurian Devonian
Approximate location of Burley No. 1 well Seismic Stratigraphic Extensional and Thrust Age West Formation or Group Name East Lithology Packages Orogenic Events Sheets Perm. Lower Upper Post-Pottsville rocks, undivided Pottsville Group and Middle post-Pottsville rocks Alleghanian orogeny Penn. Lower Pottsville Group Upper Greenbrier Limestone and Mauch Chunk Group Greenbrier Limestone Miss. Lower Berea Sandstone, Sunbury Shale, and Price Formation Venango Group Venango Group (Formation) Hampshire Formation and Riceville Formation Chagrin Shale Bradford Group Bradford Group Huron Mbr. of Greenland Gap Group the Ohio Shale Upper Salina sheet Acadian orogeny Java Formation Angola Shale Member Devonian West Falls Elk Group Formation Rhinestreet Shale Member Brallier Formation Elk Group Sonyea Formation Genesee Formation Harrell Shale Middle Tully Limestone, Hamilton Group, Marcellus Shale, and Onondaga Limestone Hamilton Group Lower Oriskany Sandstone and Helderberg Group Upper Salina Group (includes salt beds) Salina Group, Tonoloway Limestone, and Wills Creek Formation and Wills Creek Formation Salina Group Paleozoic Lockport Dolomite and Keefer Sandstone McKenzie Limestone and Keefer Sandstone Silurian Rose Hill Formation Lower Reedsville- Tuscarora Sandstone Taconic orogeny Martinsburg Juniata Formation Juniata Formation sheet Oswego Sandstone Upper Reedsville Shale (Utica Shale at base) Reedsville Shale Trenton Limestone Trenton Limestone Black River Limestone Middle Ordovician Knox unconformity Beekmantown Group Beekmantown Group ? Passive continental Lower Rome- margin modified Waynesboro Upper sandstone member of the Copper Ridge Dolomite of the Knox Group by Rome trough sheet Upper extension Copper Ridge Dolomite of the Knox Group Knox Group and Middle pre-Knox rocks Conasauga Group and Rome Formation Cambrian Lower Autochthonous Grenvillian basement Grenvillian Grenvillian basement basement Proterozoic Figure 3.--Correlation chart of Paleozoic and Proterozoic rocks in the study area and associated thrust sheets. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
Key, M. M., Jr. and N. Potter, Jr. 1992
Guidebook for the llth Annual Field Trip of the Harrisburg Area Geological Society May 9, 1992 Paleozoic Geology of the Paw Paw-Hancock Area of Maryland and West Virginia by Marcus M. Key, Jr. and Noel Potter, Jr. Dickinson College TABLE OF CONTENTS . .. List of F1gures . .............................................. 111 Introduction . ....................................... · ......... 1 Road Log • ..•... • ..... · .... • •.....•....•...•......• e ••• '0 ••••••••• 3 Stop 1. Roundtop Hill . ............ o •••••••••• o •••••••••••••••••• 5 stop 2. Sideling Hill Road Cut ..•.••............••.••••......... 8 Stop 3. Sideling Hill Diamictite Exposure ....•.•....•.•....•... 11 Stop 4. Cacapon Mountain Overlook .••.......•......•.•••••...... 15 Stop 5. Fluted Rocks Overlook .•..•••.••....•.•.•••.•........... 16 Stop 6. Fluted Rocks ................. .,. .......... ., o ••••• ., •••••• • 19 Stop 7. Berkeley Springs state Park •...•.....................•. 20 Acknowled·gments . ........................... :- ... e ••••••••••••••• 21 References .....••.•..•.•••.•..•.•..•.••......................•. 2 2 Topogrpphic maps covering field trip stops: USGS 7 1/2 minute quadrangles Bellegrove (MD-PA-WV), Great Cacapon (WV-MD), Hancock (WV-MD-PA) Cover Photo: Anticline in Silurian Bloomsburg Formation. From Stose and swartz (1912). The anticline is visible from the towpath of the c & 0 Canal at Roundtop Hill (Stop# 1). Guidebook copies may be obtained by writing: Harrisburg Area Geological Society cjo Pennsylvania Geological Survey P.O. Box 2357 Harrisburg, -
Pander Society Newsletter
Pander Society Newsletter Compiled and edited by P.H. von Bitter and J. Burke DEPARTMENT OF NATURAL HISTORY (PALAEOBIOLOGY SECTION), ROYAL ONTARIO MUSEUM, TORONTO, ONTARIO, CANADA M5S 2C6 Number 38 June 2006 www.conodont.net CHIEF PANDERER’S REMARKS Dear Conodont Colleagues: A year has gone by since I last communicated like this, and I’m pleased (and relieved) that another Pander Society Newsletter is ready to ‘go’. Thank you for having sent in your reports and questionnaires; without your willingness to going through a bit of pain there would be no Pander Society Newsletter, and our communications would be the poorer. I am very grateful to compiler and editor Joan Burke (Toronto) and webmaster Mark Purnell (Leicester) for their dedication and ongoing interest; they have helped me greatly and continue to make me look better than I really am, particularly in a time of personal and professional transition. You, the Pander Society membership, continue to ‘re-invent’ and apply conodonts in startling new ways. Some of this re-invention was seen at the Pander Society Symposium in Harrisburg, Pennsylvania, where on March 20-22, 2006 our (mostly) North American members focused on Conodonts & Sequence Stratigraphy. Looking ahead, the programme of ICOS 2006 on July 12-30/ 2006 in Leicester, England, promises not only to surprise and delight, but looks remarkably diverse and imaginative. Christian Pander, would, on the 150th anniversary of the publication of his major conodont study, no doubt be enormously impressed and pleased with the innovativeness and progress of his intellectual grandchildren. My best wishes to all of you. -
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 -
Lithostratigraphy and Petrophysics of the Devonian Marcellus Interval in West Virginia and Southwestern Pennsylvania
October 18, 2009 Lithostratigraphy and Petrophysics of the Devonian Marcellus Interval in West Virginia and Southwestern Pennsylvania Boyce, Matthew L Dept of Geology and Geography West Virginia University 98 Beechurst Ave, 330 Brooks Hall Morgantown, WV 26505 E-mail: [email protected] Carr, Timothy R Marshall Miller Professor of Geology West Virginia University 98 Beechurst Ave, 330 Brooks Hall Morgantown, WV 26505 Abstract In the Appalachian basin, the Middle Devonian organic-rich shale interval, including the Marcellus Shale, is an important target for exploration. This unconventional gas reservoir is widespread across the basin and has the potential to produce large volumes of gas (estimated to have up to 1,307 trillion cubic feet of recoverable gas). Although the Middle Devonian organic- rich shale interval has significant economic potential, stratigraphic distribution, depositional patterns and petrophysical characteristics have not been adequately characterized in the subsurface. Based on log characteristics, tied to core information, the lithostratigraphic boundaries of the Marcellus and associated units were established and correlated throughout West Virginia and southwestern Pennsylvania. Digital well logs (LAS files) were used to generate estimates of lithology and to identify zones of higher gas content across the study area. In addition, a lithologic solution was calibrated to X-ray Diffraction (XRD) data. Using previous studies on organic shale, relationships between the natural radioactivity (as measured by the gamma-ray log) were incorporated with techniques to identify gas-prone intervals. The comparison between the Uranium content and the measured bulk density identified intervals in the Marcellus with high gas saturations and were used to generate an approach to correct water saturations.