Gas Shales Report 2009 Mid-Year Mtg Revised
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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’. -
Evaluation of the Depositional Environment of the Eagle Ford
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 2012 Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas Zachary Paul Hendershott Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Earth Sciences Commons Recommended Citation Hendershott, Zachary Paul, "Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas" (2012). LSU Master's Theses. 863. https://digitalcommons.lsu.edu/gradschool_theses/863 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. EVALUATION OF THE DEPOSITIONAL ENVIRONMENT OF THE EAGLE FORD FORMATION USING WELL LOG, SEISMIC, AND CORE DATA IN THE HAWKVILLE TROUGH, LASALLE AND MCMULLEN COUNTIES, SOUTH TEXAS A Thesis Submitted to the Graduate Faculty of the Louisiana State University Agricultural and Mechanical College in partial fulfillment of the requirements for degree of Master of Science in The Department of Geology and Geophysics by Zachary Paul Hendershott B.S., University of the South – Sewanee, 2009 December 2012 ACKNOWLEDGEMENTS I would like to thank my committee chair and advisor, Dr. Jeffrey Nunn, for his constant guidance and support during my academic career at LSU. -
Eagle Ford Group and Associated Cenomanian–Turonian Strata, U.S
U.S. Gulf Coast Petroleum Systems Project Assessment of Undiscovered Oil and Gas Resources in the Eagle Ford Group and Associated Cenomanian–Turonian Strata, U.S. Gulf Coast, Texas, 2018 Using a geology-based assessment methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of 8.5 billion barrels of oil and 66 trillion cubic feet of gas in continuous accumulations in the Upper Cretaceous Eagle Ford Group and associated Cenomanian–Turonian strata in onshore lands of the U.S. Gulf Coast region, Texas. −102° −100° −98° −96° −94° −92° −90° EXPLANATION Introduction 32° LOUISIANA Eagle Ford Marl The U.S. Geological Survey (USGS) Continuous Oil AU TEXAS assessed undiscovered, technically MISSISSIPPI Submarine Plateau-Karnes Trough Continuous Oil AU recoverable hydrocarbon resources in Cenomanian–Turonian self-sourced continuous reservoirs of 30° Mudstone Continuous Oil AU the Upper Cretaceous Eagle Ford Group Eagle Ford Marl Continuous and associated Cenomanian–Turonian Gas AU Submarine Plateau–Karnes strata, which are present in the subsurface Trough Continuous Gas AU 28° across the U.S. Gulf Coast region, Texas Cenomanian–Turonian Mudstone Continuous (fig. 1). The USGS completes geology- GULF OF MEXICO Gas AU based assessments using the elements Cenomanian–Turonian 0 100 200 MILES Downdip Continuous of the total petroleum system (TPS), 26° Gas AU 0 100 200 KILOMETERS which include source rock thickness, MEXICO NM OK AR TN GA organic richness, and thermal maturity for MS AL self-sourced continuous accumulations. Base map from U.S. Department of the Interior National Park Service TX LA FL Assessment units (AUs) within a TPS Map are defined by strata that share similar Figure 1. -
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. -
U.S. Shale Gas
U.S. Shale Gas An Unconventional Resource. Unconventional Challenges. WHITE PAPER U.S. Shale Gas An Unconventional Resource . Unconventional Challenges . Executive Summary Current increasing demand and lagging supply mean high prices for both oil and gas, making exploitation of North American unconventional gas plays suddenly far more lucrative for producers. One of the most important such plays to emerge has been U.S. shale gas, with current recoverable reserves conservatively estimated at 500 to 1,000 trillion cubic feet. Hydraulic fracturing and horizontal drilling are the key enabling technologies that first made recovery of shale gas economically viable with their introduction in the Barnett Shale of Texas during the 1990s. However, a comparison of the currently hottest shale plays makes it clear that, after two decades of development and several iterations of the learning curve, best practices are application-dependent and must evolve locally. That said, a review of current trends in these hot plays indicates that, in many cases, the impact of high-drilling density required to develop continuous gas accumulations can be minimized through early and better identification of the accumulation type and size, well- designed access and transportation networks, and cooperative planning and construction efforts, when possible. U.S. Shale Gas Geographic Potential Across the U.S., from the West Coast to the Northeast, some 19 geographic basins are recognized sources of shale gas, where an estimated 35,000 wells were drilled in 2006. Presently, significant commercial gas shale production occurs in the Barnett Shale in the Fort Worth Basin, Lewis Shale in the San Juan Basin, Antrim Shale in the Michigan Basin, Marcellus Shale and others in the Appalachian Basin, and New Albany Shale in the Illinois Basin. -
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. -
Theory and Perspective on Stimulation of Unconventional Tight
Theory and Perspective on Stimulation of Unconventional Tight Oil Reservoir in China Zhifeng Luo Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University, Chengdu 610500, China; e-mail: [email protected] Yujia Gao∗ Postgraduate College of Oil and Gas Engineering, Southwest Petroleum University,Chengdu 610500, China; e-mail:[email protected] Liqiang Zhao Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University,Chengdu 610500, China; e-mail: [email protected] Pingli Liu Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University,Chengdu 610500, China; e-mail: [email protected] Nianyin Li Professor National key Laboratory of Oil and Gas Reservoir and Exploitation; College of Oil and Gas Engineering, Southwest Petroleum University, Chengdu 610500, China; e-mail: [email protected] ABSTRACT China has tremendous unconventional tight oil resources which are widely distributed in lots of petroliferous basin. However, compared with North American, all the tight oil reservoirs discovered in China has its own characteristics including continental sedimentation, interbeded formation, worse reservoir physical properties and less oil reserves per unit volume, which make it much harder to stimulate. Based on thorough analysis of successful stimulation experiences in North American, taking the characteristic of China’s tight oil reservoir into consideration, this article emphasized that increasing stimulated volume must be paid attention to, what’s more, integrated fracturing technology must be adopted into tight oil reservoir stimulation to promote both production and recovery efficiency. -
U.S. Geological Survey Fact Sheet 2020-3045
U.S. Gulf Coast Petroleum Systems Project Assessment of Undiscovered Oil and Gas Resources in the Upper Cretaceous Austin Chalk and Tokio and Eutaw Formations, U.S. Gulf Coast, 2019 Using a geology-based assessment methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of 6.9 billion barrels of oil and 41.5 trillion cubic feet of natural gas in conventional and continuous accumulations in the Upper Cretaceous Austin Chalk and Tokio and Eutaw Formations onshore and in State waters of the U.S. Gulf Coast region. Introduction Geologic Models for Assessment The U.S. Geological Survey (USGS) assessed undiscovered, The Austin Chalk, consisting of both chalk and marl, was technically recoverable oil and gas in the Upper Cretaceous deposited on a broad, low-relief marine shelf that deepened to the (Coniacian–Santonian) Austin Chalk and Tokio and Eutaw Forma- south and west during the Coniacian–Santonian marine transgression. tions in the subsurface of the Gulf Coast from southern Texas to Landward, to the northeast, the Austin Chalk transitions into sandstone the Florida Panhandle. The Austin Chalk and related stratigraphic and mudstone of the Tokio Formation in Arkansas and Louisiana and the units present onshore and in State waters of the U.S. Gulf Coast Eutaw Formation in Mississippi and Alabama. The Tokio and Eutaw region are part of the Upper Jurassic–Cretaceous–Tertiary Composite Formations were deposited in shallow to marginal marine depositional Total Petroleum System (TPS) (Condon and Dyman, 2006). environments at the leading edge of the marine transgression. The source of hydrocarbons in Austin Chalk, Tokio, and Eutaw reservoirs 100° 98° 96° 94° 92° 90° 88° 86° varies spatially throughout the onshore Gulf Coast. -
Diagenesis in the Upper Cretaceous Eagle Ford Shale
DIAGENESIS IN THE UPPER CRETACEOUS EAGLE FORD SHALE, SOUTH TEXAS by Allison Schaiberger Copyright by Allison Schaiberger (2016) All Rights Reserved A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date ______________________ Signed: ____________________________________ Allison Schaiberger Signed: ____________________________________ Dr. Steve Sonnenberg Thesis Advisor Signed: ____________________________________ Dr. Stephen Enders Interim Department Head Department of Geology and Geological Engineering Golden, Colorado Date ______________________ ii ABSTRACT This study utilizes three cores provided by Devon Energy from LaVaca and Dewitt Counties, TX, which were analyzed with a focus on diagenetic fabrics within the Lower Eagle Ford. A better understanding of paragenesis within the organic-rich Lower Eagle Ford was developed with the use of XRF and XRD measurements, thin section samples, stable isotope analysis, and CL analysis. The majority of diagenetic alteration occurred early at shallow depths within anoxic/suboxic environments and slightly sulfate-reducing conditions from diagenetic fluids with varying isotopic composition. Diagenetic expression variation is most influenced by the depositional facies in which alteration occurs. Within the study area, four identified depositional facies (A-D), and five diagenetic facies (1-5) were identified within the Lower Eagle Ford study area based -
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 Models and Evaluation of Undiscovered Conventional and Continuous Oil and Gas Resources— Upper Cretaceous Austin Chalk, U.S
Geologic Models and Evaluation of Undiscovered Conventional and Continuous Oil and Gas Resources— Upper Cretaceous Austin Chalk, U.S. Gulf Coast Scientific Investigations Report 2012–5159 U.S. Department of the Interior U.S. Geological Survey Front Cover. Photos taken by Krystal Pearson, U.S. Geological Survey, near the old Sprinkle Road bridge on Little Walnut Creek, Travis County, Texas. Geologic Models and Evaluation of Undiscovered Conventional and Continuous Oil and Gas Resources—Upper Cretaceous Austin Chalk, U.S. Gulf Coast By Krystal Pearson Scientific Investigations Report 2012–5159 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: Pearson, Krystal, 2012, Geologic models and evaluation of undiscovered conventional and continuous oil and gas resources—Upper Cretaceous Austin Chalk, U.S.