U.S. Geological Survey Open-File Report Series 2006-1237

Total Page:16

File Type:pdf, Size:1020Kb

U.S. Geological Survey Open-File Report Series 2006-1237 Assessment of Appalachian Basin Oil and Gas Resources: Devonian Shale–Middle and Upper Paleozoic Total Petroleum System By Robert C. Milici and Christopher S. Swezey Open-File Report Series 2006-1237 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Dirk A. Kempthorne, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 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 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. 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. 2 Contents Abstract ......................................................................................................................................9 Acknowledgments ......................................................................................................................9 Introduction…………………………………………………………………….…..……….…...9 Stratigraphy…………………………………………………………………….…..……….….10 Devonian stable shelf……………………………………………………..……….…..10 The Acadian delta……………………………………………………..……….… .......12 The regional facies model...................................................................12 The Catskill delta................................................................................13 Middle Devonian strata…………………………………….…13 Hamilton Group and equivalent strata.......................13 Tully Limestone.........................................................14 Regional unconformity ..............................................14 Upper Devonian and Lower Mississippian strata...................14 Post-unconformity Devonian and Mississippian black gas shales..........................................................14 Brallier Formation and equivalent strata ...................16 Price-Rockwell (Pocono) delta ...........................................................17 Definition and distribution .....................................................17 Price Formation…………………………………….… ..........17 Virginia and southern West Virginia .........................17 Northern West Virginia, Maryland, and Pennsylvania ..............................................................18 Progradational delta deposits.....................................19 Patton Shale Member.................................................20 Sea level transgression and unconformities ...............20 Burgoon and Purslane Formations……………………………21 Maccrady Fomration ..............................................................21 The Berea delta...................................................................................22 Mississippian stable shelf ............................................................................................22 Upper Mississippian Greenbrier/Newman Limestones...................................22 Tennessee, southwestern Virginia, eastern Kentucky, and southern West Virginia.....................................................................................23 Northern West Virginia ......................................................................23 Pennsylvania and Maryland................................................................23 Ohio ....................................................................................................24 Regional isopach.................................................................................24 Petroleum geology....................................................................................................................25 General.........................................................................................................................25 The assessment model.....................................................................................25 Thermal maturation data .................................................................................25 Petroleum system events .................................................................................26 Devonian Shale–Middle and Upper Paleozoic total petroleum system.......................27 Part I: Continuous oil and gas resources .........................................................27 Greater Big Sandy Assessment Unit (GBS AU) ................................28 Introduction ............................................................................28 Stratigraphy ............................................................................28 3 Greater Big Sandy Assessment Unit (GBS AU) )–Continued Geologic structure ..................................................................29 Devonian shale as a source rock for methane ........................29 Gas-in-place data....................................................................30 Thermal maturity, hydrocarbon generation, and migration....30 Reservoir and production data................................................31 Greater Big Sandy AU fields and pools .................................31 Assessment results..................................................................31 Northwestern Ohio Shale Assessment Unit (NWOS AU)..................31 Introduction ............................................................................31 Stratigraphy ............................................................................32 Geologic structure ..................................................................32 Devonian shale as a source rock for methane ........................33 Gas-in-place data....................................................................33 Thermal maturity, hydrocarbon generation, and migration....34 Reservoir and production data................................................34 Northwestern Ohio Shale AU fields and pools ......................35 Assessment results..................................................................35 Devonian Siltstone and Shale Assessment Unit (DSS AU) ...............35 Introduction ............................................................................35 Stratigraphy ............................................................................35 Geologic structure ..................................................................36 Devonian shale as a source rock for methane ........................36 Gas-in-place data....................................................................36 Thermal maturity, hydrocarbon generation, and migration....37 Reservoir and production data................................................37 Devonian Siltstone and Shale fields and pools ......................37 Assessment results..................................................................38 Marcellus Shale Assessment Unit (MS AU) ......................................38 Introduction ............................................................................38 Stratigraphy ............................................................................38 Geologic structure ..................................................................38 Devonian shale as a source rock for methane ........................38 Gas-in-place data....................................................................39 Thermal maturity, hydrocarbon generation, and migration....39 Marcellus Shale fields and pools............................................39 Assessment results..................................................................39 Catskill Sandstone and Siltstone Assessment Unit.............................39 Introduction ............................................................................39 Stratigraphy ............................................................................40 Depositional environments.....................................................40 Petroleum system model ........................................................40 Catskill fields and pools .........................................................41 Assessment results..................................................................41 Berea Sandstone Assessment Unit......................................................42 Introduction ............................................................................42 Stratigraphy ............................................................................42 Depositional environments.....................................................42 4 Berea Sandstone Assessment Unit–Continued Petroleum system model ........................................................43 Berea Sandstone fields and pools...........................................43 Assessment results..................................................................43 Part II: Conventional oil and gas resources.....................................................44 The Oriskany Sandstone Stratigraphic and Structural Assessment Units....................................................................................................44 Introduction ............................................................................44
Recommended publications
  • FISHING for DUNKLEOSTEUS You’Re Definitely Gonna Need a Bigger Boat by Mark Peter
    OOhhiioo GGeeoollooggyy EEXXTTRRAA July 31, 2019 FISHING FOR DUNKLEOSTEUS You’re definitely gonna need a bigger boat by Mark Peter At an estimated maximum length of 6 to 8.8 meters (20–29 sediments that eroded from the Acadian Mountains, combined feet), Dunkleosteus terrelli (Fig. 1) would have been a match for with abundant organic matter from newly evolved land plants even the Hollywood-sized great white shark from the and marine plankton, settled in the basin as dark organic movie Jaws. Surfers, scuba divers, and swimmers can relax, muds. Over millions of years, accumulation of additional however, because Dunkleosteus has been extinct for nearly 360 overlying sediments compacted the muds into black shale rock. million years. Dunkleosteus was a placoderm, a type of armored The rocks that formed from the Late Devonian seafloor fish, that lived during the Late Devonian Period from about sediments (along with fossils of Dunkleosteus) arrived at their 375–359 million years ago. Fossil remains of the large present location of 41 degrees north latitude after several species Dunkleosteus terrelli are present in the Cleveland hundred million years of slow plate tectonic movement as the Member of the Ohio Shale, which contains rocks that are North American Plate moved northward. approximately 360–359 million years old. Figure 1. A reconstruction of a fully-grown Dunkleosteus terrelli, assuming a length of 29 feet, with angler for scale. Modified from illustration by Hugo Salais of Metazoa Studio. Dunkleosteus cruised Late Devonian seas and oceans as an Figure 2. Paleogeographic reconstruction of eastern North America during apex predator, much like the great white shark of today.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Geological Investigations in Ohio
    INFORMATION CIRCULAR NO. 21 GEOLOGICAL INVESTIGATIONS IN OHIO 1956 By Carolyn Farnsworth STATE OF OHIO C. William O'Neill, Governor DEPARTMENT OF NATURAL RESOURCES A. W. Marion, Director NATURAL RESOURCES COMMISSION Milton Ronsheim, Chairman John A. Slipher, Bryce Browning, Vice Chairman Secretary C. D. Blubaugh Dean L. L. Rummell Forrest G. Hall Dr. Myron T. Sturgeon A. W. Marion George Wenger DIVISION OF GEOLOGICAL SURVEY Ralph J. Bernhagen, Chief STATI OF OHIO DIPAlTMIMT 011 NATUlAL llSOUlCH DIVISION OF &EOLO&ICAL SURVEY INFORMATION CIRCULAR NO. 21 'GEOLOG·ICAL INVESTIGATIONS IN OHIO 1956 by CAROLYN FARNSWORTH COLUMBUS 1957 Blank Page CONTENTS Page Introduction 1 Project listing by author 2 Project listing by subject . 22 Economic geology 22 Aggregates . 22 Coal . • 22 Ground water 22 Iron .. 22 Oil and gas 22 Salt . 22 Sand and gravel 23 General .. 23 Geomorphology 23 Geophysics 23 Glacial geology 23 Mineralogy and petrology . 24 Clay .. 24 Coal . 24 Dolomite 24 Limestone. 24 Sandstone •• 24 Shale. 24 Till 25 Others 25 Paleontology. 25 Stratigraphy and sedimentation 26 Structural geology . 27 Miscellaneous . 27 Geographic distribution. 27 Statewide 27 Areal. \\ 28 County 29 Miscellaneous . 33 iii Blank Page I INTRODUCTION In September 1956, letters of inquiry and questionnaires were sent to all Ohio geologists on the mailing list of the Ohio Geological Survey, and to other persons who might be working on geological problems in Ohio. This publication has been compiled from the information contained on the returned forms. In most eases it is assumed that the projects listed herein will culminate in reports which will be available to the profession through scientific journals, government publications, or grad- uate school theses.
    [Show full text]
  • Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
    SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present.
    [Show full text]
  • Guide to the Geology of Northeastern Ohio
    SDMS US EPA REGION V -1 SOME IMAGES WITHIN THIS DOCUMENT MAY BE ILLEGIBLE DUE TO BAD SOURCE DOCUMENTS. GUIDE TO THE GEOLOGY of NORTHEASTERN OHIO Edited by P. O. BANKS & RODNEY M. FELDMANN 1970 Northern Ohio Geological Society ELYP.i.A PU&UC LIBRARt as, BEDROCK GEOLOGY OF NORTHEASTERN OHIO PENNSYLVANIAN SYSTEM MISSISSIPPIAN SYSTEM DEVONIAN SYSTEM \V&fe'£:i£:VS:#: CANTON viSlSWSSWM FIGURr I Geologic map of northeastern Ohio. Individual formations within each time unit are not dis- -guished, and glacial deposits have been omitted. Because the bedding planes are nearly ••.crizontal, the map patterns of the contacts closely resemble the topographic contours at those z evations. The older and deeper units are most extensively exposed where the major rivers rave cut into them, while the younger units are preserved in the intervening higher areas. CO «< in Dev. Mississippian r-c Penn. a> 3 CO CD BRADF. KINOERHOOK MERAMEC —1 OSAGE CHESTER POTTSVIUE ro to r-» c-> e-> e= e-i GO n « -n V) CO V* o ^_ ^ 0. = -^ eo CO 3 c= « ^> <C3 at ta B> ^ °» eu ra to a O9 eo ^ a* s 1= ca \ *** CO ^ CO to CM v» o' CO to CO 3 =3 13- *•» \ ¥\ A. FIGURE 1. Columnar section ol the major stratigraphic units in northeastern Ohio showing their relative positions in the standard geologic time scale. The Devonian-Mississippian boundary is not known with certainty to lie within the Cleveland Shale. The base of the Mississippian in the northern part of the state is transitional with the Bradford Series of the Devonian System and may lie within the Cleveland Shale (Weller er a/., 1948).
    [Show full text]
  • Geoloaic District. Subsequent Stratigraphic Studies in This Area
    DEVONIAN STRATA AND PALEOENVIRONMENTS: CHAUTAUQUA COUNTY REGION: NEW YORK STATE GORDON C. BAIRD and GARY G. LASH Department of Geosciences State University of New York College at Fredonia Fredonia, New York 14063 INTRODUCTION The history of the study of the Paleozoic stratigraphic divisions in New York State spans, at least, two centuries, and it records the early development of important concepts centrally germane to the study of sedimentary basins worldwide (see Tesmer, 1989). The works of James Hall, John Clarke, HenryS. Williams, Joseph Barrell, and George Chadwick are well known to most sedimentary workers, as are those of numerous subsequent workers. In particular, the sedimentary sequences of the Allegheny Plateau Region (••southern Tier" region) served as important sources of information for refinement of the fac ies concept ar.d for the widespread recognition of the westwardly prograding Catskill Delta Complex which is the primary Paleozoic story recorded in Southern Tier bedrock deposits (see Chadwick, 1924, 1933; Cooper, et al., 1942; Caster, 1934; Woodrow, 1985). ---- The first significant geologic work relating to the Chautauqua County region was presented in James Hall's (1843) Survey of the Fourth Geoloaic District. Subsequent stratigraphic studies in this area inclu e Clarke (1903), Chadwick (1923, 1924), Caster (1934), Pepper and de Witt (1950, 1951) and de Witt and Colton (1953). In northwest Pennsylvania, significant synthetic contributions include I.C. White (1881), Butts (1906-1908), Chadwick (1925), Caster ·(1934), Pepper et al. (1954). In Ohio, deposits equivalent to parts of the New York and -­ Pennsylvania Upper Devonian section (Chagrin Shale) have been the subject of recent paleoenvironmental studies (see Weidner and Feldmann, 1983; Schwimmer and Feldmann, 1990).
    [Show full text]
  • Geologic Cross Section
    Geologic Cross Section I–I′ Through the Appalachian Basin from the Eastern Margin of the Illinois Basin, Jefferson County, Kentucky, to the Valley and Ridge Province, Scott County, Virginia By Robert T. Ryder, Michael H. Trippi, and Christopher S. Swezey Pamphlet B to accompany Scientific Investigations Map 3343 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copy- righted items must be secured from the copyright owner. Suggested citation: Ryder, R.T., Trippi, M.H., and Swezey, C.S., 2015, Geologic cross section I–I′ through the Appalachian basin from the eastern margin of the Illinois basin, Jefferson County, Kentucky, to the Valley and Ridge province, Scott County, Virginia: U.S. Geological Survey Scientific Investigations Map 3343, 2 sheets and pamphlet A, 41 p.; pamphlet B, 102 p., http://dx.doi.org/10.3133/sim3343.
    [Show full text]
  • GEOLOGIC SUMMARY of the APPALACHIAN BASIN, with REFERENCE to the SUBSURFACE DISPOSAL of RADIOACTIVE WASTE SOLUTIONS by George W
    TEI-791 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY" GEOLOGIC SUMMARY OF THE APPALACHIAN BASIN, WITH;REFERENCE TO THE SUBSURFACE DISPOSAL OF RADIOACTIVE WASTE SOLUTIONS* By George W. Colton June 1961 Report TEI-791 This report is preliminary and ha^;not been edited for conformity with G^logical Survey format and nomenclature. ?1 ^Prepared on behalf of the U. S. Atomic Energy Commission. CONTENTS Abstract* .......................... 5 Introduction. ........................ 7 Purpose of report. ................... 7 Organization of report .................. 7 Location and extent of area. .............. Q Acknowledgments. .................... 10 Geologic framework. ..................... 10 Depositional framework ................. 10 Structural framework .................. llj. Stratigraphy. ........................ 17 Late Precambrian stratified sequence .......... 17 Early Cambrian clastic sequence. ............ 18 Thickness and depth ................ 22 Cambrian-Ordovician carbonate sequence ......... 23 Thickness and depth . , ........... 35 Late Ordovician clastic sequence ............ 35 Thickness and depth ................ Mi- Early Silurian clastic sequence. ............ kk Thickness and depth ................ 51 Silurian-Devonian carbonate sequence .......... 52 Thickness and depth ................ 62 Devonian classic sequence. ............... 63 Thickness and depth ................ 69 Mississippian sequence ................. 70 Thickness and depth ................ 79 Pennsylvanian sequence ................. 79 Waste
    [Show full text]
  • Geologic Cross Section C–C' Through the Appalachian Basin from Erie
    Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 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 more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov 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 materials contained within this report. Suggested citation: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p.
    [Show full text]
  • 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.
    [Show full text]
  • Outcrop Lithostratigraphy and Petrophysics of the Middle Devonian Marcellus Shale in West Virginia and Adjacent States
    Graduate Theses, Dissertations, and Problem Reports 2011 Outcrop Lithostratigraphy and Petrophysics of the Middle Devonian Marcellus Shale in West Virginia and Adjacent States Margaret E. Walker-Milani West Virginia University Follow this and additional works at: https://researchrepository.wvu.edu/etd Recommended Citation Walker-Milani, Margaret E., "Outcrop Lithostratigraphy and Petrophysics of the Middle Devonian Marcellus Shale in West Virginia and Adjacent States" (2011). Graduate Theses, Dissertations, and Problem Reports. 3327. https://researchrepository.wvu.edu/etd/3327 This Thesis is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Outcrop Lithostratigraphy and Petrophysics of the Middle Devonian Marcellus Shale in West Virginia and Adjacent States Margaret E. Walker-Milani THESIS submitted to the College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Master of Science in Geology Richard Smosna, Ph.D., Chair Timothy Carr, Ph.D. John Renton, Ph.D. Kathy Bruner, Ph.D.
    [Show full text]