Review of Emerging Resources: U.S. Shale Gas and Oil Plays
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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. -
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. -
Stratigraphic Evaluation of the St. Joe-Boone Boundary Interval
University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 8-2018 Stratigraphic Evaluation of the St. Joe-Boone Boundary Interval, Kinderhookian-Osagean Series, Lower Mississippian System, Tri-State Region, Southern Midcontinent Forrest Dalton McFarlin University of Arkansas, Fayetteville Follow this and additional works at: https://scholarworks.uark.edu/etd Part of the Geology Commons, and the Stratigraphy Commons Recommended Citation McFarlin, Forrest Dalton, "Stratigraphic Evaluation of the St. Joe-Boone Boundary Interval, Kinderhookian-Osagean Series, Lower Mississippian System, Tri-State Region, Southern Midcontinent" (2018). Theses and Dissertations. 2952. https://scholarworks.uark.edu/etd/2952 This Thesis is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Stratigraphic Evaluation of the St. Joe-Boone Boundary Interval, Kinderhookian-Osagean Series, Lower Mississippian System, Tri-State Region, Southern Midcontinent A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by Forrest Dalton McFarlin Texas Christian University Bachelor of Science in Geology, 2015 August 2018 University of Arkansas This thesis is approved for recommendation to the Graduate Council. _____________________________________ Walter Manger, PhD Thesis Director _____________________________________ Adriana Potra, PhD Committee Member _____________________________________ Thomas McGilvery, PhD Committee Member ©2018 by Forrest Dalton McFarlin All Rights Reserved Abstract The Lower Mississippian interval comprises a single, third-order, eustatic cycle subdivided lithostratigraphically into the St. Joe Limestone (Hopkins 1893) and overlying Boone Formation (Branner 1891, Simonds 1891) with type areas in northern Arkansas. -
Bedrock Geology of Altenburg Quadrangle, Jackson County
BEDROCK GEOLOGY OF ALTENBURG QUADRANGLE Institute of Natural Resource Sustainability William W. Shilts, Executive Director JACKSON COUNTY, ILLINOIS AND PERRY COUNTY, MISSOURI STATEMAP Altenburg-BG ILLINOIS STATE GEOLOGICAL SURVEY E. Donald McKay III, Interim Director Mary J. Seid, Joseph A. Devera, Allen L. Weedman, and Dewey H. Amos 2009 360 GEOLOGIC UNITS ) ) ) 14 Qal Alluvial deposits ) 13 18 Quaternary Pleistocene and Holocene 17 360 ) 15 360 16 14 0 36 ) 13 Qf Fan deposits ) Unconformity Qal ) & 350 tl Lower Tradewater Formation Atokan ) ) Pennsylvanian 360 ) &cv Caseyville Formation Morrowan 24 360 ) Unconformity ) 17 Upper Elviran undivided, Meu ) Waltersburg to top of Degonia 19 20 Qal 21 22 23 ) 24 ) Mv Vienna Limestone 360 o ) 3 Mts ) 350 Mts Tar Springs Sandstone ) 20 360 ) Mgd 360 30 ) Mgd Glen Dean Limestone ) 21 350 360 Mts 29 ) Qal Hardinsburg Sandstone and J N Mhg Chesterian ) Golconda Formations h Æ Qal Mav anc 28 27 Br ) N oJ 26 25 JN 85 N ) Cypress Sandstone through J Mcpc Dsl 500 Paint Creek Formation JN N ) J o Mts N 5 J s ) Dgt 600 J N 70 J N Mgd Yankeetown Formation s ) Myr Db 80 28 Æ and Renault Sandstone N J 29 N J N ) Sb J Mgd Mississippian o Dgt Ssc 25 Clines o N 25 Msg 27 ) Qal J 80 s 3 Mav Aux Vases Sandstone N J N Mts o MILL J MISSISSIPPI 34 ) Qal J N ) N J Dsl 35 N 26 J o N 25 J Mgd Mgd ) Msg Ste. Genevieve Limestone 500 o Db DITCH J 20 Mgd N N N ) J J o RIVER o N 600 J 80 N ) 10 o J Mav Æ Msl St. -
Financial Research & Analysis
Financial Research & Analysis Oil and Gas Accounting Hot Topics 2009 Webcast March 12, 2009 Julie Hilt Hannink [email protected] + 301.354.9919 Today’s Agenda Commodity Price Drives Impairment Charges Borrowing Bases and Covenant Compliance Modernization of SEC Reserve Disclosure LIFO Repeal and Other US Budget Proposals www.riskmetrics.com 2 Commodity Price Plunge Drove Impairments in 4Q08 Relative lack of impairments and price-related impairment charges over the past 6-7 years due to rising oil prices and decent natural gas price trends. Period end pricing most important for Full Cost (FC) companies as ceiling test charges based on those prices. This will change with new SEC rules as it goes to 12-month average. Although 3Q06 and 4Q06 were problematic on the natural gas price front, improved price by report date meant limited impairments in those quarters. Chart 1: Quarterly Closing Oil and Natural Gas Prices 2001-2008 - Price Plunge Expected to Affect Reserve Estimates and Impairments $160 $16 Oil -WTI $140 Natural Gas - HH $14 $120 $12 $100 $10 Natural gas price average $6.13/mcf $80 $8 North Slope $60 US Lower 48 $6 $40 $4 $20 Oil price average $53.26/bbl $2 $0 $0 1Q01 3Q01 1Q02 3Q02 1Q03 3Q03 1Q04 3Q04 1Q05 3Q05 1Q06 3Q06 1Q07 3Q07 1Q08 3Q08 Source: NYMEX, RiskMetrics analysis www.riskmetrics.com 3 Full Cost Ceiling Test Charge Risk Fulfilled Based on high capital spending during the first part of 2009 meant high risk of impairments for companies listed in Chart 2. Significant in the table below are SGY which took $1.3 billion ($850 million AT) impairment charge plus another $466 million in goodwill impairment after spending up for Bois D’Arc and HK which took a $951 million ($600 million AT) impairment charge. -
Long-Range Petroleum Migration in the Illinois Basin CRAIG M
ILLINOIS STATE GEOLOGICAL SURVEY Interior Cratonic Basins, 1991, edited by Reprint Series 1991 - T26 M. W. Leighton, D. R. Kalata, D. F. Oltz, and J. J. Eidel: American Association of Petroleum Geologists Memoir 51,819 p. CHAPTER 26 Long-Range Petroleum Migration in the Illinois Basin CRAIG M. BETHKE DONALD F. OLTZ University of Illinois Illinois State Geological Survey Urbana, Illinois Champaign, Illinois JACKIE D. REED ARCO Oil and Gas Company Plano, Texas Editor's note: No treatment of oil and gas in the Illinois In this section, we define the migration that has basin would be complete without an overview of occurred in the Illinois basin on the basis of shale hydrocarbon migration. The following is a condensed petrographic observations and geochemical correla version, made especially for this volume, of an article tions. We emphasize the origin of oils found in shallow that will appear in the American Association of reservoirs, mostly in Silurian strata to the north and Petroleum Geologists Bulletin in 1991. northwest of the central basin (Figure 26-2), because these oils seem to have migrated farthest from source beds. We show that these oils, which are produced from reservoirs more than 125 mi (200 km) from the basin's depocenter, were derived from Devonian source rocks in the deep basin. We then use quantitative models of the basin's paleohydrology to INTRODUCTION investigate the past subsurface conditions that drove the migration. We conclude that long-range migration The distribution of petroleum production from the was not related to processes occurring as the basin Illinois basin extends considerably beyond the area subsided and infilled. -
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. -
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. -
Bossier Bossier
CENTER FOR ENERGY STUDIES BOSSIER - HAYNESVILLE SHALE: NORTH LOUISIANA SALT BASIN D. A. GODDARD, E. A. MANCINI, S. C. TALUKAR & M. HORN Louisiana State University Baton Rouge , Louisiana 1 OVERVIEW Regional Geological Setting Total Organic Carbon & RockRock--EvalEval Pyrolisis Kerogen Petrography Thin Section Petrography Naturally Fractured Shale Reservoirs Conclusions 2 Gulf Coast Interior Basins Gulf Coast Interior Salt Basins Mancini and Puckett, 2005 3 TYPE LOG 4 Type Wells 5 Bossier Parish Wells 6 BossierBossier--HaynesvilleHaynesville samples in NLSB . (LA Parish) Sample (Serial #) OP/Well Name Core Interval Depth-Ft (Jackson) 10,944 (162291) AMOCO Davis Bros. Bossier Fm. 10, 945 10,948 Haynesville Fm. 12,804 12,956 12,976 (164798) AMOCO CZ 5-7 (Winn) 15,601 Bossier Fm. 15, 608 Haynesville Fm. 16,413 16,418 16,431 16,432 (166680) EXXON Pardee (Winn) 16195 Bossier Fm. 16, 200 16,400 (107545) Venzina Green #1 (Union) 9,347 Bossier Fm. 9,357 9,372 7 8 Bossier -Haynesville samples in Vernon Field Serial. # Operator Well Field Sec TWP RGE Parish Sample Depth- Ft 224274 Anadarko Fisher 16 #1 Vernon 16 16N 02W Jackson 13,175 13,770 226742 Anadarko Davis Bros 29 Vernon 29 16N 02W Jackson 14,035 15,120 231813 Anadarko Beasley 9 #2 Vernon 9 16N 02W Jackson 11,348 232316 Anadarko StewtHarrison Vernon 34 16N 03W Jackson 11,805 34 #2 9 Modified from Structuremaps.com 10 11 12 13 Analytical results of Total Organic Carbon, RockRock--EvalEval PyrolysisPyrolysis,, and Vitrinite Reflectance (Ro) in the NLSB. Depth % TOC Wt S1 S2 S3 Well Sample (Ft) % mg/g mg/g mg/g Tmax HI OI S1/TOC PI TAI Ro AMOCO DAVIS Cotton V. -
Chesapeake Energy Arena
PROJECT PROFILE Chesapeake Energy Arena Designed by Jerrold Stevens of Marsh/PMK Installed by Ford AV Project Details Location Oklahoma City, Oklahoma Category Sports (arena) Project Type 18,200-seat indoor arena Fulcrum Products (32) CS121 21 inch Subcardioid Subwoofers Supporting Products EAW Anya Speaker Modules Lab.gruppen Power Amplifiers The Chesapeake Energy Arena, Oklahoma City’s premier venue for large events and QSC Q-SYS Core DSP entertainment, is primarily known as the home of the NBA’s Oklahoma City Thunder. Renkus-Heinz STX Series Speakers The Arena modernized its sound system prior to the Thunder’s 2016-17 season with the Yamaha CL3 Digital Mixing Console first large scale deployment of Fulcrum’s CS121 passive cardioid subwoofers and the NBA’s first permanent installation of EAW’s Anya adaptive-array system. Designed by Marsh/ PMK’s Jerrold Stevens and installed by Ford AV, the advanced technology audio solution gives the Oklahoma City Thunder a sound to match their name. Challenges “The sound system needed excellent intelligibility, fidelity, output and bandwidth to enhance the overall fan experience and become more competitive with other NBA arenas, ” Stevens explains. Solution “Cardioid was a huge factor in the arena design,” Stevens says. “Vertical subwoofer arrays are ideal for providing smooth coverage to the seating bowl and keeping sound energy off the floor. However, the large centrally located scoreboard precluded any loudspeakers directly over center court. Forced to hang subwoofer arrays around the scoreboard’s perimeter, I knew cardioid patterns were necessary to minimize interference between arrays.” Stevens was familiar with Fulcrum’s passive cardioid line array modules and their ability to eliminate excessive rear low frequency radiation without requiring additional drivers, amplifiers or signal processing channels.