Update on North America Shale-Gas Exploration and Development
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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’. -
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. -
Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and Adjacent
Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and AdJa(-erit Parts of the Lewis Sliale and Lance Formation, East Flank of the Rock Springs Uplift, Southwest lo U.S. OEOLOGI AL SURVEY PROFESSIONAL PAPER 1532 Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and Adjacent Parts of the Lewis Shale and Lance Formation, East Flank of the Rock Springs Uplift, Southwest Wyoming By HENRYW. ROEHLER U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1532 Description of three of/lapping barrier shorelines along the western margins of the interior seaway of North America UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director 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 Roehler, Henry W. Stratigraphy of the Upper Cretaceous Fox Hills sandstone and adjacent parts of the Lewis shale and Lance formation, east flank of the Rock Springs Uplift, southwest Wyoming / by Henry W. Roehler. p. cm. (U.S. Geological Survey professional paper ; 1532) Includes bibliographical references. Supt.ofDocs.no.: I19.16:P1532 1. Geology, Stratigraphic Cretaceous. 2. Geology Wyoming. 3. Fox Hills Formation. I. Geological Survey (U.S.). II. Title. III. Series. QE688.R64 1993 551.7T09787 dc20 92-36645 CIP For sale by USGS Map Distribution Box 25286, Building 810 Denver Federal Center Denver, CO 80225 CONTENTS Page Page Abstract......................................................................................... 1 Stratigraphy Continued Introduction................................................................................... 1 Formations exposed on the east flank of the Rock Springs Description and accessibility of the study area ................ -
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. -
Central San Juan Basin
Acta - ---- - - ---Palaeontologic- -- ---' ~ Polonica Vol. 28, No. 1-2 pp. 195-204 Warszawa, 1983 Second Symposium on Mesozoic Terrestiol. Ecosystems, Jadwisin 1981 SPENCER G. LUCAS and NIALL J. MATEER VERTEBRATE PALEOECOLOGY OF THE LATE CAMPANIAN (CRETACEOUS):FRUITLAND FORMATION, SAN JUAN BASIN, ~EW MEXICO (USA) LUCAS, s. G. and MATEER, N. J .: Vertebrate paleoecology of the late Campanian (Cretaceous) Fruitland Formation, San Juan Basin, New Mexico (USA). Acta Palaeontologica Polonica, 28, 1-2, 195-204, 1983. Sediments of the Fruitland Formation in northwestern New Mexico represent a delta plain that prograded northeastward over the retrating strandline of the. North American epeiric seaway during the late Campanian. Fruitland fossil · vertebrates are fishes, amphibians, lizards, a snake, turtles, crocodilians, dinosaurs (mostly h adrosaurs and ceratopsians) and mammals. Autochthonous fossils in the Fruitland ' Form ation represent organisms of the trophically-complex Para saurolophus community. Differences in diversity, physical stress and life-history strategies within the ParasaurolopllUS community . fit well the stablllty-time hypothesis. Thus, dinosaurs experienced relatively low physical stress whereas fishes, amphibians, small reptiles and mammals experienced greater physical stress. Because of this, dinosaurs were less likely to recover from an environment al catastrophe than were smaller contemporaneous vertebrates. The terminal Cretaceous extinctions selectively eliminated animals that lived in less physlcally -stressed situations, indicating that the extinctions resulted from an environmental catastrophe. Key w 0 r d s: Fruitland Formation, New Mexico, delta plain, stablllty-time hypothesis, Cretaceous extinctions. Spencer G. Lucas, Department ot Geology and Geophysics and Peabody Museum ot Natural History, Yale University, P.O. Box 6666, New Haven, Connecticut 06511 USA ; NlaU J . -
Technically Recoverable Shale Oil and Shale Gas Resources: United Kingdom
Technically Recoverable Shale Oil and Shale Gas Resources: United Kingdom September 2015 Independent Statistics & Analysis U.S. Department of Energy www.eia.gov Washington, DC 20585 September 2015 This report was prepared by the U.S. Energy Information Administration (EIA), the statistical and analytical agency within the U.S. Department of Energy. By law, EIA’s data, analyses, and forecasts are independent of approval by any other officer or employee of the United States Government. The views in this report therefore should not be construed as representing those of the Department of Energy or other Federal agencies. U.S. Energy Information Administration | Technically Recoverable Shale Oil and Shale Gas Resources i September 2015 Contents Executive Summary ....................................................................................................................................... 3 Introduction ............................................................................................................................................. 3 Resource categories ................................................................................................................................. 3 Methodology ........................................................................................................................................... 5 Key exclusions .......................................................................................................................................... 6 United Kingdom…………………………………… ………………………………………………………………………………………......XI-1 -
Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations
Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-A Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations By HENRY W. ROEHLER GEOLOGY OF THE EOCENE WASATCH, GREEN RIVER, AND BRIDGER (WASHAKIE) FORMATIONS, GREATER GREEN RIVER BASIN, WYOMING, UTAH, AND COLORADO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director 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 Roehler, Henry W. Introduction to greater Green River basin geology, physiography, and history of investigations / by Henry W. Roehler. p. cm. (Geology of the Eocene Wasatch, Green River, and Bridger (Washakie) formations, greater Green River basin, Wyoming, Utah, and Colorado) (U.S. Geological Survey professional paper ; 1506-A) Includes bibliographical references (p. ). Supt. of Docs, no.: I 19.16:1506A 1. Geology, Stratigraphic Eocene. 2. Geology Green River Watershed (Wyo.-Utah). I. Title. II. Series. III. Series: U.S. Geological Survey professional paper ; 1506-A. QE692.2.R625 1992 551.7'84'097925 dc20 91-23181 CIP For sale by Book and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Abstract ........................................................................................................................................ Al Purpose and scope of investigation ............................................................................................ 1 Location and accessibility of the greater Green River basin ................................................... 2 Geologic setting ........................................................................................................................... -
Application of Organic Petrography in North American Shale Petroleum Systems: a Review
International Journal of Coal Geology 163 (2016) 8–51 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Application of organic petrography in North American shale petroleum systems: A review Paul C. Hackley a, Brian J. Cardott b a U.S. Geological Survey, MS 956 National Center, 12201 Sunrise Valley Dr, Reston, VA 20192, USA b Oklahoma Geological Survey, 100 E. Boyd St., Rm. N-131, Norman, OK 73019-0628, USA article info abstract Article history: Organic petrography via incident light microscopy has broad application to shale petroleum systems, including Received 13 April 2016 delineation of thermal maturity windows and determination of organo-facies. Incident light microscopy allows Received in revised form 10 June 2016 practitioners the ability to identify various types of organic components and demonstrates that solid bitumen Accepted 13 June 2016 is the dominant organic matter occurring in shale plays of peak oil and gas window thermal maturity, whereas Available online 16 June 2016 oil-prone Type I/II kerogens have converted to hydrocarbons and are not present. High magnification SEM obser- Keywords: vation of an interconnected organic porosity occurring in the solid bitumen of thermally mature shale reservoirs Organic petrology has enabled major advances in our understanding of hydrocarbon migration and storage in shale, but suffers Thermal maturity from inability to confirm the type of organic matter present. Herein we review organic petrography applications Shale petroleum systems in the North American shale plays through discussion of incident light photographic examples. In the first part of Unconventional resources the manuscript we provide basic practical information on the measurement of organic reflectance and outline Vitrinite reflectance fluorescence microscopy and other petrographic approaches to the determination of thermal maturity. -
Mesozoic Stratigraphy at Durango, Colorado
160 New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin, 2005, p. 160-169. LUCAS AND HECKERT MESOZOIC STRATIGRAPHY AT DURANGO, COLORADO SPENCER G. LUCAS AND ANDREW B. HECKERT New Mexico Museum of Natural History and Science, 1801 Mountain Rd. NW, Albuquerque, NM 87104 ABSTRACT.—A nearly 3-km-thick section of Mesozoic sedimentary rocks is exposed at Durango, Colorado. This section con- sists of Upper Triassic, Middle-Upper Jurassic and Cretaceous strata that well record the geological history of southwestern Colorado during much of the Mesozoic. At Durango, Upper Triassic strata of the Chinle Group are ~ 300 m of red beds deposited in mostly fluvial paleoenvironments. Overlying Middle-Upper Jurassic strata of the San Rafael Group are ~ 300 m thick and consist of eolian sandstone, salina limestone and siltstone/sandstone deposited on an arid coastal plain. The Upper Jurassic Morrison Formation is ~ 187 m thick and consists of sandstone and mudstone deposited in fluvial environments. The only Lower Cretaceous strata at Durango are fluvial sandstone and conglomerate of the Burro Canyon Formation. Most of the overlying Upper Cretaceous section (Dakota, Mancos, Mesaverde, Lewis, Fruitland and Kirtland units) represents deposition in and along the western margin of the Western Interior seaway during Cenomanian-Campanian time. Volcaniclastic strata of the overlying McDermott Formation are the youngest Mesozoic strata at Durango. INTRODUCTION Durango, Colorado, sits in the Animas River Valley on the northern flank of the San Juan Basin and in the southern foothills of the San Juan and La Plata Mountains. Beginning at the northern end of the city, and extending to the southern end of town (from north of Animas City Mountain to just south of Smelter Moun- tain), the Animas River cuts in an essentially downdip direction through a homoclinal Mesozoic section of sedimentary rocks about 3 km thick (Figs.