U.S. Shale Gas
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Deconstructing the Fayetteville Lessons from a Mature Shale Play
Deconstructing the Fayetteville ©Lessons Kimmeridge 2015 from - Deconstructing a Mature the Fayetteville Shale Play June 20151 Introduction The Fayetteville shale gas play lies in the eastern Arkoma Basin, east of the historic oil and gas fields in the central and western parts of the Basin. As one of the most mature, well-developed and well-understood shale gas plays, it offers an unparalleled dataset on which we can look back and review how closely what we “thought we knew” matches “what we now know”, and what lessons there are to be learned in the development of shales and the distribution of the cores of these plays. As we have previously noted (see Figure 1), identifying the core of a shale play is akin to building a Venn diagram based on a number of geological factors. By revisiting the Fayetteville we can rebuild this diagram and overlay it on what is now a vast database of historical wells to see whether it matched expectations, and if not, why not. The data also allows us to review how the development of the play changed (lateral length, completion, etc.) and the variance in performance Figure 1: Schematic of gradational overlap of geologic between operators presents valuable lessons in attributes that define the core of an unconventional whether success is all about the rocks, or whether resource play operator knowledge/insight can make good rocks bad or vice versa. © Kimmeridge 2015 - Deconstructing the Fayetteville 2 Background The Fayetteville shale lies in the eastern Arkoma Basin and ranges in depth from outcrop in the north to 9,000’ at the southern end of the play, with drill depths primarily between 3,000’ and 6,000’. -
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. -
Study Develops Fayetteville Shale Reserves, Production Forecast John Browning Katie Smye a Study of Reserve and Production Potential for the Fayette- Scott W
Study develops Fayetteville Shale reserves, production forecast John Browning Katie Smye A study of reserve and production potential for the Fayette- Scott W. Tinker Susan Horvath ville Shale in north central Arkansas forecasts a cumulative Svetlana Ikonnikova Tad Patzek 18 tcf of economically recoverable reserves by 2050, with Gürcan Gülen Frank Male production declining to about 400 bcf/year by 2030 from Eric Potter Forrest Roberts the current peak of about 950 bcf/year. Qilong Fu Carl Grote The forecast suggests the formation will continue to be a The University of Texas major contributor to U.S. natural gas production. Austin The Bureau of Economic Geology (BEG) at The University In this cross section of the Fayetteville Shale, the pay zone is identified by lines correlated between logs. Shaded areas of density-log porosity (DPhi) curve represent DPhi values less than 5%. The map shows the location of the cross section. TECHNOLOGY 1 FAYETTEVILLE POROSITY * THICKNESS (PHI*H) FIG. 2 Contours,2 density porosity-ft Stone 5 8 11 14 17 20 23 26 29 32 35 38 41 44 47 50 Batesville Van Buren Cleburne Independence Pope Conway Faulkner Area shown White Conway 0 Miles 25 Arkansas 0 Km 40 1With 60° NE trend bias to reect fault trends. 2Porosity is net from density logs (DPhi). of Texas at Austin conducted the study, integrating engineer- sient flow model for the first 3-5 years, resulting in decline ing, geology, and economics into a numerical model that al- rates inversely proportional to the square root of time, later lows for scenario testing on the basis of an array of technical shifting to exponential decline as a result of interfracture and economic parameters. -
Shallow Groundwater Quality and Geochemistry in the Fayetteville Shale Gas-Production Area, North-Central Arkansas, 2011
Prepared in cooperation with (in alphabetical order) the Arkansas Natural Resources Commission, Arkansas Oil and Gas Commission, Duke University, Faulkner County, Shirley Community Development Corporation, and the University of Arkansas at Fayetteville, and the U.S. Geological Survey Groundwater Resources Program Shallow Groundwater Quality and Geochemistry in the Fayetteville Shale Gas-Production Area, North-Central Arkansas, 2011 Scientific Investigations Report 2012–5273 U.S. Department of the Interior U.S. Geological Survey Cover: Left, Drilling rig and equipment used in the Fayetteville Shale gas-production area, north-central Arkansas. Right, Pond with synthetic liner used to store water at shale gas-production facility in the Fayetteville Shale area, north-central Arkansas. Bottom, Freshwater pond and distribution lines for source water used in drilling and hydrofracturing in the Fayetteville Shale gas-production area, north-central Arkansas. All photographs by Timothy M. Kresse, U.S. Geological Survey. Shallow Groundwater Quality and Geochemistry in the Fayetteville Shale Gas-Production Area, North-Central Arkansas, 2011 By Timothy M. Kresse, Nathaniel R. Warner, Phillip D. Hays, Adrian Down, Avner Vengosh, Robert B. Jackson Prepared in cooperation with (in alphabetical order) the Arkansas Natural Resources Commission, Arkansas Oil and Gas Commission, Duke University, Faulkner County, Shirley Community Development Corporation, and the University of Arkansas at Fayetteville, and the U.S. Geological Survey Groundwater Resources Program Scientific Investigations Report 2012–5273 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 This and other USGS information products are available at http://store.usgs.gov/ U.S. -
EVIDENCE of PRESSURE DEPENDENT PERMEABILITY in LONG-TERM SHALE GAS PRODUCTION and PRESSURE TRANSIENT RESPONSES a Thesis by FABIA
EVIDENCE OF PRESSURE DEPENDENT PERMEABILITY IN LONG-TERM SHALE GAS PRODUCTION AND PRESSURE TRANSIENT RESPONSES A Thesis by FABIAN ELIAS VERA ROSALES Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Approved by: Chair of Committee, Christine Ehlig-Economides Committee Members, Robert Wattenbarger Maria Barrufet Head of Department, Dan Hill December 2012 Major Subject: Petroleum Engineering Copyright 2012 Fabian Elias Vera Rosales ABSTRACT The current state of shale gas reservoir dynamics demands understanding long- term production, and existing models that address important parameters like fracture half-length, permeability, and stimulated shale volume assume constant permeability. Petroleum geologists suggest that observed steep declining rates may involve pressure- dependent permeability (PDP). This study accounts for PDP in three potential shale media: the shale matrix, the existing natural fractures, and the created hydraulic fractures. Sensitivity studies comparing expected long-term rate and pressure production behavior with and without PDP show that these two are distinct when presented as a sequence of coupled build-up rate-normalized pressure (BU-RNP) and its logarithmic derivative, making PDP a recognizable trend. Pressure and rate field data demonstrate evidence of PDP only in Horn River and Haynesville but not in Fayetteville shale. While the presence of PDP did not seem to impact the long term recovery forecast, it is possible to determine whether the observed behavior relates to change in hydraulic fracture conductivity or to change in fracture network permeability. As well, it provides insight on whether apparent fracture networks relate to an existing natural fracture network in the shale or to a fracture network induced during hydraulic fracturing. -
Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction by MACKENZIE GORDON, JR
Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction By MACKENZIE GORDON, JR. Corals By WILLIAM J. SANDO Pelecypods By JOHN POJETA, JR. Gastropods By ELLIS L. YOCHELSON Trilobites By MACKENZIE GORDON, JR. Ostracodes By I. G. SOHN GEOLOGICAL SURVEY PROFESSIONAL PAPER 606-A, B, C, D, E, F Papers illustrating and describing certain of G. H. Girty' s invertebrate fossils from the Fayetteville Shale UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-650224 For sale by the Superintendent of Documents, U.S. Government Printing Office Washing.ton, D.C. 20402 CONTENTS [The letters in parentheses preceding the titles are those used to designate the chapters] Page (A) Introduction, by Mackenzie Gordon, Jr _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 1 (B) Corals, by William J. Sando__________________________________________________________________________________ 9 (C) Pelecypods, by John Pojeta, Jr _____ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 15 (D) Gastropods, by Ellis L. -
Geologic and Geochemical Studies of the New Albany Shale Group (Devonian-Mississippian) in Illinois
557 3M SuMr IL6of 1980-2 Final Report Geologic and Geochemical Studies of the New Albany Shale Group (Devonian-Mississippian) in Illinois R. E. Bergstrom and N. F. ShimP/ Principal Invistigators Robert M. Cluff, Project Coordinator Illinois State Geological Survey Open File Series 1980-2 June 30, 1980 Illinois State Geological Survey Urbana, IL 61801 Prepared for U.S. Department of Energy Morgantown Energy Technology Center Morgantown, WV 2 6505 Contract: U.S. Department of Energy DE-AC21-76ET12142 , Note to readers: Printouts of the data contained on the computer file and copies of the structure map mentioned in this report can be obtained from the Illinois State Geological Survey upon written request, This report was prepared as an account of work partially sponsored by the U.S. Government. Neither the United States nor the United States Depart- ment of Energy, nor any of their employees , contractors, subcontractors or employees makes any warranty, express 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 privately owned rights. '^'NOIS STATE QEOLOQICAL SURVEY 3 305 Final Report Geologic and Geochemical Studies of the New Albany Shale Group (Devonian-Mississippian) in Illinois R. E. Bergstrom and N. F. Shimp, Principal Invistigators Robert M. Cluff, Project Coordinator Illinois State Geological Survey Open File Series 1980-2 SEP 1 1 1996 |L uluu ourWtY June 30, 1980 Illinois State Geological Survey Urbana, IL 61801 Prepared for U.S. Department of Energy Morgantown Energy Technology Center Morgantown, WV 2 6505 Contract: U.S. -
Permian Basin, West Texas and Southeastern New Mexico
Report of Investigations No. 201 Stratigraphic Analysis of the Upper Devonian Woodford Formation, Permian Basin, West Texas and Southeastern New Mexico John B. Comer* *Current address Indiana Geological Survey Bloomington, Indiana 47405 1991 Bureau of Economic Geology • W. L. Fisher, Director The University of Texas at Austin • Austin, Texas 78713-7508 Contents Abstract ..............................................................................................................................1 Introduction ..................................................................................................................... 1 Methods .............................................................................................................................3 Stratigraphy .....................................................................................................................5 Nomenclature ...................................................................................................................5 Age and Correlation ........................................................................................................6 Previous Work .................................................................................................................6 Western Outcrop Belt ......................................................................................................6 Central Texas ...................................................................................................................7 Northeastern Oklahoma -
The Influence of Vertical Location on Hydraulic Fracture Conductivity In
THE INFLUENCE OF VERTICAL LOCATION ON HYDRAULIC FRACTURE CONDUCTIVITY IN THE FAYETTEVILLE SHALE A Thesis by KATHRYN ELIZABETH BRIGGS Submitted to the Office of Graduate and Professional Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Chair of Committee, Ding Zhu Committee Members, A. Daniel Hill Michael Pope Head of Department, A. Daniel Hill May 2014 Major Subject: Petroleum Engineering Copyright 2014 Kathryn Elizabeth Briggs ABSTRACT Hydraulic fracturing is the primary stimulation method within low permeability reservoirs, in particular shale reservoirs. Hydraulic fracturing provides a means for making shale reservoirs commercially viable by inducing and propping fracture networks allowing gas flow to the wellbore. Without a propping agent, the created fracture channels would close due to the in-situ stress and defeat the purpose of creating induced fractures. The fracture network conductivity is directly related to the well productivity; therefore, the oil and gas industry is currently trying to better understand what impacts fracture conductivity. Shale is a broad term for a fine-grained, detrital rock, composed of silts and clays, which often suggest laminar, fissile structure. This work investigates the difference between two vertical zones in the Fayetteville shale, the FL2 and FL3, by measuring laboratory fracture conductivity along an artificially induced, rough, aligned fracture. Unpropped and low concentration 30/70 mesh proppant experiments were run on samples from both zones. Parameters that were controllable, such as proppant size, concentration and type, were kept consistent between the two zones. In addition to comparing experimental fracture conductivity results, mineral composition, thin sections, and surface roughness scans were evaluated to distinguish differences between the two zones rock properties. -
B2150-B FRONT Final
Bedrock Geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Kentucky, and Missouri By W. John Nelson THE PADUCAH CUSMAP QUADRANGLE: RESOURCE AND TOPICAL INVESTIGATIONS Martin B. Goldhaber, Project Coordinator T OF EN TH TM E U.S. GEOLOGICAL SURVEY BULLETIN 2150–B R I A N P T E E R D . I O S . R A joint study conducted in collaboration with the Illinois State Geological U Survey, the Indiana Geological Survey, the Kentucky Geological Survey, and the Missouri M 9 Division of Geology and Land Survey A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Schaefer, Acting Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Nelson, W. John Bedrock geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Ken- tucky, and Missouri / by W. John Nelson. p. cm.—(U.S. Geological Survey bulletin ; 2150–B) (The Paducah CUSMAP Quadrangle, resource and topical investigations ; B) Includes bibliographical references. Supt. of Docs. no. : I 19.3:2150–B 1. Geology—Middle West. I. Title. II. Series. III. Series: The Paducah CUSMAP Quadrangle, resource and topical investigations ; B QE75.B9 no. 2150–B [QE78.7] [557.3 s—dc21 97–7724 [557.7] CIP CONTENTS Abstract .......................................................................................................................... -
Gas Exploration in the Devonian Shales of Kentucky
ISSN 0075-5559 KENTUCKY GEOLOGICAL SURVEY UNIVERSITY OF KENTUCKY, LEXINGTON Donald C. Haney, State Geologist and Director GAS EXPLORATION IN THE DEVONIAN SHALES OF KENTUCKY Terence Hamilton-Smith Front coverGeophysical logs of a frac- tured gas reservoir in the New Albany Shale in western Kentucky. BULLETIN 4 Series XI, 1993 UNIVERSITY OF KENTUCKY GEOLOGICAL DIVISION Charles T. Wethington, Jr., President Coal and Minerals Section: Linda J. Magid, Vice President for Research and James C. Cobb, Head Graduate Studies Garland R. Dever, Jr., Geologist VII Jack Supplee, Director, Fiscal Affairs and Sponsored Donald R. Chesnut, Jr., Geologist V Project Administration Cortland F. Eble, Geologist V David A. Williams, Geologist V, Henderson Office KENTUCKY GEOLOGICAL SURVEY ADVISORY Warren H. Anderson, Geologist IV BOARD Gerald A. Weisenfluh, Geologist IV Steve Cawood, Chairman, Pineville Stephen F. Greb, Geologist III Larry R. Finley, Henderson Robert Andrews, Geologist I Hugh B. Gabbard, Richmond Kenneth Gibson, Madisonville Petroleum and Stratigraphy Section: Wallace W. Hagan, Lexington James A. Drahovzal, Head Phil M. Miles, Lexington Martin C. Noger, Geologist VII W. A. Mossbarger, Lexington Terence Hamilton-Smith, Geologist V Ralph Palmer, Winchester Patrick J. Gooding, Geologist IV Henry A. Spalding, Hazard David C. Harris, Geologist IV Ralph N. Thomas, Owensboro Brandon C. Nuttall, Geologist IV George H. Warren, Jr., Owensboro Matthew Humphreys, Geologist II David A. Zegeer, Lexington Mara Chen, Post-Doctoral Scholar James B. Harris, Post-Doctoral Scholar KENTUCKY GEOLOGICAL SURVEY Robert R. Daniel, Laboratory Technician B Donald C. Haney, State Geologist and Director Anna E. Watson, Staff Assistant IV John D. Kiefer, Assistant State Geologist for Adminis- Frances A. -
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