A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin
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Modern Shale Gas Development in the United States: a Primer
U.S. Department of Energy • Office of Fossil Energy National Energy Technology Laboratory April 2009 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. Modern Shale Gas Development in the United States: A Primer Work Performed Under DE-FG26-04NT15455 Prepared for U.S. Department of Energy Office of Fossil Energy and National Energy Technology Laboratory Prepared by Ground Water Protection Council Oklahoma City, OK 73142 405-516-4972 www.gwpc.org and ALL Consulting Tulsa, OK 74119 918-382-7581 www.all-llc.com April 2009 MODERN SHALE GAS DEVELOPMENT IN THE UNITED STATES: A PRIMER ACKNOWLEDGMENTS This material is based upon work supported by the U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory (NETL) under Award Number DE‐FG26‐ 04NT15455. Mr. Robert Vagnetti and Ms. Sandra McSurdy, NETL Project Managers, provided oversight and technical guidance. -
Hydraulic Fracturing in the Barnett Shale
Hydraulic Fracturing in the Barnett Shale Samantha Fuchs GIS in Water Resources Dr. David Maidment University of Texas at Austin Fall 2015 Table of Contents I. Introduction ......................................................................................................................3 II. Barnett Shale i. Geologic and Geographic Information ..............................................................6 ii. Shale Gas Production.........................................................................................7 III. Water Resources i. Major Texas Aquifers ......................................................................................11 ii. Groundwater Wells ..........................................................................................13 IV. Population and Land Cover .........................................................................................14 V. Conclusion ....................................................................................................................16 VI. References....................................................................................................................17 2 I. Introduction Hydraulic Fracturing, or fracking, is a process by which natural gas is extracted from shale rock. It is a well-stimulation technique where fluid is injected into deep rock formations to fracture it. The fracking fluid contains a mixture of chemical components with different purposes. Proppants like sand are used in the fluid to hold fractures in the rock open once the hydraulic -
Assessing Undiscovered Resources of the Barnett-Paleozoic Total Petroleum System, Bend Arch–Fort Worth Basin Province, Texas* by Richard M
Assessing Undiscovered Resources of the Barnett-Paleozoic Total Petroleum System, Bend Arch–Fort Worth Basin Province, Texas* By Richard M. Pollastro1, Ronald J. Hill1, Daniel M. Jarvie2, and Mitchell E. Henry1 Search and Discovery Article #10034 (2003) *Online adaptation of presentation at AAPG Southwest Section Meeting, Fort Worth, TX, March, 2003 (www.southwestsection.org) 1U.S. Geological Survey, Denver, CO 2Humble Geochemical Services, Humble, TX ABSTRACT Organic-rich Barnett Shale (Mississippian-Pennsylvanian) is the primary source rock for oil and gas that is produced from Paleozoic reservoir rocks in the Bend Arch–Fort Worth Basin Province. Areal distribution and geochemical typing of hydrocarbons in this mature petroleum province indicates generation and expulsion from the Barnett at a depocenter coincident with a paleoaxis of the Fort Worth Basin. Barnett-sourced hydrocarbons migrated westward into reservoir rocks of the Bend Arch and Eastern shelf; however, some oil and gas was possibly sourced by a composite Woodford-Barnett total petroleum system of the Midland Basin from the west. Current U.S. Geological assessments of undiscovered oil and gas are performed using the total petroleum system (TPS) concept. The TPS is composed of mature source rock, known accumulations, and area(s) of undiscovered hydrocarbon potential. The TPS is subdivided into assessment units based on similar geologic characteristics, accumulation type (conventional or continuous), and hydrocarbon type (oil and (or) gas). Assessment of the Barnett-Paleozoic TPS focuses on the continuous (unconventional) Barnett accumulation where gas and some oil are produced from organic-rich siliceous shale in the northeast portion of the Fort Worth Basin. Assessment units are also identified for mature conventional plays in Paleozoic carbonate and clastic reservoir rocks, such as the Chappel Limestone pinnacle reefs and Bend Group conglomerate, respectively. -
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. -
Chapter 4 GEOLOGY
Chapter 4 GEOLOGY CHAPTER 4 GEOLOGY ...................................................................................................................................... 4‐1 4.1 INTRODUCTION ................................................................................................................................................ 4‐2 4.2 BLACK SHALES ................................................................................................................................................. 4‐3 4.3 UTICA SHALE ................................................................................................................................................... 4‐6 4.3.2 Thermal Maturity and Fairways ...................................................................................................... 4‐14 4.3.3 Potential for Gas Production ............................................................................................................ 4‐14 4.4 MARCELLUS FORMATION ................................................................................................................................. 4‐15 4.4.1 Total Organic Carbon ....................................................................................................................... 4‐17 4.4.2 Thermal Maturity and Fairways ...................................................................................................... 4‐17 4.4.3 Potential for Gas Production ........................................................................................................... -
Road Log of the Geology of Frederick County, Virginia W
Vol. 17 MAY, 1971 No. 2 ROAD LOG OF THE GEOLOGY OF FREDERICK COUNTY, VIRGINIA W. E. Nunan The following road log is a guide to geologic The user of this road log should keep in mind features along or near main roads in Frederick that automobile odometers vary in accuracy. Dis- County, Virginia. Distances and cumulative mile- tances between stops and road intersections ages between places where interesting and repre- should be checked frequently, especially at junc- sentative-lithologies, formational contacts, struc- tions or stream crossings immediately preceding tural features, fossils, and geomorphic features stops. The Frederick County road map of the occur are noted. At least one exposure for nearly Virginia Department of Highways, and the U. S. each formation is included in the log. Brief dis- Geological Survey 7.5-minute topographic maps cussions of the geological features observable at are recommended for use with this road log. the various stops is included in the text. Topographic maps covering Frederick County include Boyce, Capon Bridge, Capon Springs, A comprehensive report of the geology of the Glengary, Gore, Hayfield, Inwood, Middletown, Mountain Falls, Ridge, Stephens City, Stephen- County is presented in "Geology and Mineral Re- son, Wardensville, White Hall, and Winchester. sources of Frederick County" by Charles Butts The route of the road log (Figure 1) shows U. S. and R. S. Edmundson, Bulletin 80 of the Virginia and State Highways and those State Roads trav- Division of Mineral Resources. The publication eled or needed for reference at intersections. has a 1:62,500 scale geologic map in color, which Pertinent place names, streams, and railroad is available from the Division for $4.00 plus sales crossings are indicated. -
3. Natural Gas
UNIVERSITY OF GOTHENBURG Department of Earth Sciences Geovetarcentrum/Earth Science Centre Unconventional gas and oil - in the USA and Poland Jakub Leśniewicz ISSN 1400-3821 C90 Project Göteborg 2012 Mailing address Address Telephone Telefax Geovetarcentrum Geovetarcentrum Geovetarcentrum 031-786 19 56 031-786 19 86 Göteborg University S 405 30 Göteborg Guldhedsgatan 5A S-405 30 Göteborg SWEDEN Unconventional gas and oil – in the USA and Poland Jakub Leśniewicz, University of Gothenburg, Department of Earth Sciences; Geology, Box 460, SE-405 30 Göteborg Abstract Despite the fact that the exploitation of natural gas from unconventional deposits is much more difficult and less economically viable than from the conventional reservoirs, they are now a very attractive target. This is due to the gradual depletion of conventional resources, and large deposits of natural gas in unconventional reservoirs, which previously were not known or there was no technology that allows to explore them. Coalbed methane , tight gas and shale gas have been successfully developed in the United States over the past two decades. The initial increase in the production of unconventional gas, shale gas in particular, was then maintained through the use of horizontal drilling and hydraulic fracturing, as well as an increase in gas prices. Production of shale gas has a greater deposits potential, while lower productivity and higher cost of drilling, as compared to conventional gas, which is associated with a more cautious investment strategies. Shale gas exploration strategies are also different from those of conventional gas and, initially, require an extensive source rock analysis and a big land position to identify “sweet spots”. -
Exhibit 5 Town of Barton Geology and Seismicity Report Sections
GEOLOGY AND SEISMICITY REPORT SNYDER E1-A WELL TOWN OF BARTON TIOGA COUNTY, NEW YORK Prepared for: Couch White, LLP 540 Broadway P.O. Box 22222 Albany, New York 12201 Prepared by: Continental Placer Inc. II Winners Circle Albany, New York 12205 July 25, 2017 Table of Contents 1.0 EXECUTIVE SUMMARY............................................................................................................. 1 2.0 INTRODUCTION ........................................................................................................................... 2 2.1 Depositional Sequences and General Stratigraphic Sequence ................................................ 2 2.1.1 Upper Devonian Lithologies ........................................................................................................ 4 2.1.2 Marcellus-Hamilton ..................................................................................................................... 4 2.1.3 Tristates-Onondaga ...................................................................................................................... 4 2.1.4 Helderberg .................................................................................................................................... 4 2.1.5 Oneida-Clinton-Salina ................................................................................................................. 4 2.1.6 Black River-Trenton-Utica-Frankfort .......................................................................................... 5 2.1.7 Potsdam-Beekmantown .............................................................................................................. -
TXOGA Versus Denton
FILED: 11/5/2014 9:08:57 AM SHERRI ADELSTEIN Denton County District Clerk By: Amanda Gonzalez, Deputy CAUSE NO. __________14-08933-431 TEXAS OIL AND GAS ASSOCIATION, § IN THE DISTRICT COURT OF § Plaintiff, § vs. § § DENTON COUNTY, TEXAS CITY OF DENTON, § § Defendant. § § § _____ JUDICIAL DISTRICT § ORIGINAL PETITION The Texas Oil and Gas Association (“TXOGA”) files this declaratory action and request for injunctive relief against the City of Denton, on the ground that a recently-passed City of Denton ordinance, which bans hydraulic fracturing and is soon to take effect, is preempted by Texas state law and is therefore unconstitutional. I. INTRODUCTION This case concerns a significant question of Texas law: whether a City of Denton ordinance that bans hydraulic fracturing is preempted by the Constitution and laws of the State of Texas. The ordinance, approved by voters at the general election of November 4, 2014, exceeds the limited authority of home-rule cities and represents an impermissible intrusion on the exclusive powers granted by the Legislature to state agencies, the Texas Railroad Commission (the “Railroad Commission”) and the Texas Commission on Environmental Quality (the “TCEQ”). TXOGA, therefore, seeks a declaration that the ordinance is invalid and unenforceable. To achieve its overriding policy objective of the safe, efficient, even-handed, and non-wasteful development of this State’s oil and gas resources, the Texas Legislature vested regulatory power over that development in the Railroad Commission and the TCEQ. Both agencies are staffed with experts in the field who apply uniform regulatory controls across Texas and thereby avoid the inconsistencies that necessarily result from short-term political interests, funding, and turnover in local government. -
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. -
The Geology of the Lyndonville Area, Vermont
THE GEOLOGY OF THE LYNDONVILLE AREA, VERMONT By JOHN G. DENNIS VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, Stale Geologist Published by VERMONT DEVELOPMENT COMMISSION MONTPELIER, VERMONT BULLETIN NO. 8 1956 Lake Willoughby, seen from its north shore. TABLE OF CONTENTS ABSTRACT ......................... 7 INTRODUCTION 8 Location 8 Geologic Setting ..................... 8 Previous Work ...................... 8 Purpose of Study ..................... 9 Method of Study 10 Acknowledgments . 11 Physiography ...................... 11 STRATIGRAPHY ....................... 16 Lithologic Descriptions .................. 16 Waits River Formation ................. 16 General Statement .................. 16 Distribution ..................... 16 Age 17 Lithological Detail .................. 17 Gile Mountain Formation ................ 19 General Statement .................. 19 Distribution ..................... 20 Lithologic Detail ................... 20 The Waits River /Gile Mountain Contact ........ 22 Age........................... 23 Preliminary Remarks .................. 23 Early Work ...................... 23 Richardson's Work in Eastern Vermont .......... 25 Recent Detailed Mapping in the Waits River Formation. 26 Detailed Work in Canada ................ 28 Relationships in the Connecticut River Valley, Vermont and New Hampshire ................... 30 Summary of Presently Held Opinions ........... 32 Discussion ....................... 32 Conclusions ...................... 33 STRUCTURE 34 Introduction and Structural Setting 34 Terminology ...................... -
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.