Fort Berthold Oil and Gas Plays
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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. -
Bakken – the Biggest Oil Resource in the United States?
Winter 2011 Oil & Natural Gas Program Newsletter Bakken – The Biggest Oil Resource in the United States? The announcement of the acquisition of large acreage positions in the Bakken play has become a fairly regular event. Leasing activity in the Bakken has exploded over the last five years and bonus payments per acre CONTENTS have jumped. Total lease bonus payments exceeded $100 million in 2009 (Figure 1). Bakken – The Biggest Oil Resource in the United States? ...1 The heightened acquisition activity is driven by the Bakken’s immense potential. In 2008, the United States Geological Survey (USGS) estimated Commentary ...................................2 that the U.S. portion of the Bakken formation contains between 3 and 4.3 Successful Oil Production in billion barrels (a mean of 3.63 billion barrels) of undiscovered, recoverable the Bakken Formation .................6 oil, ranking it among the very largest U.S. oil plays. The Bakken—An Unconventional Petroleum The number of producing wells and Reservoir System ................9 and volume of oil production has Crude Souring in the Bakken ....11 grown with the growth in leasing and drilling (Figure 2). Production Geomechanical Study has reached nearly 8 million barrels of the Bakken .................................13 per month from roughly 4500 Bakken Requires Outlet for producing wells. Increased Production ................. 16 E&P Snapshots ............................ 18 The Bakken Formation Upcoming Meetings and The Bakken petroleum system is Presentations ............................... 20 part of a larger depositional system CONTACTS laid down in the Williston Basin during the Phanerozoic period with Roy Long Figure 1: Lease payments in North Dakota’s portion sediments up to 16,000 feet thick. -
Cumulative Index North Dakota Historical Quarterly Volumes 1-11 1926 - 1944
CUMULATIVE INDEX NORTH DAKOTA HISTORICAL QUARTERLY VOLUMES 1-11 1926 - 1944 A Aiton, Arthur S., review by, 6:245 Alaska, purchase of, 6:6, 7, 15 A’Rafting on the Mississipp’ (Russell), rev. of, 3:220- 222 Albanel, Father Charles, 5:200 A-wach-ha-wa village, of the Hidatsas, 2:5, 6 Albert Lea, Minn., 1.3:25 Abandonment of the military posts, question of, Albrecht, Fred, 2:143 5:248, 249 Alderman, John, 1.1:72 Abbey Lake, 1.3:38 Aldrich, Bess Streeter, rev. of, 3:152-153; Richard, Abbott, Johnston, rev. of, 3:218-219; Lawrence, speaker, 1.1:52 speaker, 1.1:50 Aldrich, Vernice M., articles by, 1.1:49-54, 1.4:41- Abe Collins Ranch, 8:298 45; 2:30-52, 217-219; reviews by, 1.1:69-70, Abell, E. R, 2:109, 111, 113; 3:176; 9:74 1.1:70-71, 1.2:76-77, 1.2:77, 1.3:78, 1.3:78-79, Abercrombie, N.Dak., 1.3: 34, 39; 1.4:6, 7, 71; 2:54, 1.3:79, 1.3:80, 1.4:77, 1.4:77-78; 2:230, 230- 106, 251, 255; 3:173 231, 231, 231-232, 232-233, 274; 3:77, 150, Abercrombie State Park, 4:57 150-151, 151-152, 152, 152-153, 220-222, 223, Aberdeen, D.T., 1.3:57, 4:94, 96 223-224; 4:66, 66-67, 67, 148, 200, 200, 201, Abraham Lincoln, the Prairie Years (Sandburg), rev. of, 201, 202, 202, 274, 275, 275-276, 276, 277-278; 1.2:77 8:220-221; 10:208; 11:221, 221-222 Abstracts in History from Dissertations for the Degree of Alexander, Dr. -
Evolution of Oil Production in the Bakken Formation
EvolutionEvolution ofof OilOil ProductionProduction inin thethe BakkenBakken FormationFormation JulieJulie A.A. LeFeverLeFever NorthNorth DakotaDakota GeologicalGeological SurveySurvey PlaysPlays ofof thethe BakkenBakken FormationFormation ¾¾ ConventionalConventional BakkenBakken (pre(pre--1987)1987) ¾¾ CycleCycle 11 –– AntelopeAntelope StructureStructure (1950s(1950s –– 60s)60s) ¾¾ CycleCycle 22 –– DepositionalDepositional EdgeEdge (1970s(1970s –– 80s)80s) ¾¾ HorizontalHorizontal DrillingDrilling ofof thethe BakkenBakken ShaleShale (post(post--1987)1987) ¾¾ HorizontalHorizontal DrillingDrilling ofof thethe BakkenBakken MiddleMiddle MemberMember (2001(2001 toto present)present) ConventionalConventional BakkenBakken CycleCycle 11 –– AntelopeAntelope FieldField ¾¾DiscoveryDiscovery WellWell ¾¾ StanolindStanolind -- #1#1 WoodrowWoodrow StarrStarr ¾¾ InitialInitial PotentialPotential (536(536 BO;BO; 0.10.1 BW)BW) ¾¾ AntelopeAntelope FieldField ¾¾ 5252 wells;wells; 12.512.5 millionmillion BO;BO; 1010 BCFBCF GasGas ¾¾ ““SanishSanish SandSand”” ¾¾ CompletionCompletion MethodMethod Conventional Bakken Exploration between Cycles ¾¾ElkhornElkhorn RanchRanch ¾¾ ShellShell OilOil Co.Co. -- #41X#41X--55--11 GovernmentGovernment ¾¾NessonNesson AnticlineAnticline ¾¾ #1#1 B.E.B.E. HoveHove ¾¾ IPIP -- 756756 BOPD,BOPD, 33 BWPDBWPD ¾¾ CompletionCompletion MethodMethod ConventionalConventional BakkenBakken CycleCycle 22 –– DepositionalDepositional LimitLimit ¾¾StratigraphyStratigraphy && StructureStructure ¾¾ ThinThin BakkenBakken ¾¾ MultipleMultiple PaysPays -
Ennis 30 X 60 Text–MBMG
GEOLOGIC MAP OF THE ENNIS 30' x 60' QUADRANGLE MADISON AND GALLATIN COUNTIES, MONTANA, AND PARK COUNTY, WYOMING by Karl S. Kellogg* and Van S. Williams* Montana Bureau of Mines and Geology Open-File Report 529 2006 * U. S. Geological Survey, Denver, CO Revisions by MBMG This report has been reviewed for conformity with Montana Bureau of Mines & Geology’s technical and editorial standards. Introductory Note This geologic quadrangle map is based almost entirely on the original map by Karl S. Kellogg and Van S. Williams (2000) published by the U.S. Geological Survey as Geologic Investigation Series I-2690, scale 1:100,000. Differences from the original map arise from MBMG’s effort to integrate the Ennis quadrangle data with adjacent MBMG quadrangle maps to establish a seamless geologic coverage in southwest Montana. To this end, some map unit letter symbols have been revised, twelve new units have been added, two units have been dropped, and a few unit text descriptions have been slightly modified. 1 Kalispell MONTANA 15 Great Falls 90 Missoula Helena 94 Butte Bozeman Billings 90 90 15 112°00' R3W R2W R1W R1E R2E R3E R4E R5E 111°00' 45°30' R n o s T4S 287 i d a 191 Mc Allister M Ennis TOBACCO ROOT Lake MOUNTAINS T5S r MADISON CO CO GALLATIN C Ja te ck ni C ra r G Ennis Virginia T6S City 287 A Big Sky CO PARK ld Big Sky e r Meadow Village C Mountain Village r GALLATIN CO GALLATIN G M r C a k a c l o d R T7S l i a s Cameron t o Bea i r C n n r GALLATIN RANGE GRAVELLY R 287 R i i v v RANGE e MADISON RANGE r e T8S Indian Cr r ylor Fo r Ta k R ub r y C T9S R by 191 Ru 45°00' 0246 mile 0 2 46 8 km Figure 1. -
L'.3350 Deposmon and DISSOLUTION of the MIDDLE DEVONIAN PRAIRIE FORMATION, Williston BASIN, NORTH DAKOTA and MONTANA By
l'.3350 DEPOsmON AND DISSOLUTION OF THE MIDDLE DEVONIAN PRAIRIE FORMATION, WilLISTON BASIN, NORTH DAKOTA AND MONTANA by: Chris A. Oglesby T-3350 A thesis submined 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 f:" /2 7 /C''i::-- i ; Signed: Approved: Lee C. Gerhard Thesis Advisor Golden, Colorado - 7 Date' .' Samuel S. Adams, Head Department of Geology and Geological Engineering II T-3350 ABSTRACf Within the Williston basin, thickness variations of the Prairie Formation are common and are interpreted to originate by two processes, differential accumulation of salt during deposition, and differential removal of salt by dissolution. Unambiguous evidence for each process is rare because the Prairie/Winnipegosis interval is seldom cored within the U.S. portion of the basin. Therefore indirect methods, utilizing well logs, provide the principal method for identifying characteristics of the two processes. The results of this study indicate that the two processes can be distinguished using correlations within the Prairie Formation. Several regionally correlative upward-brining, and probably shoaling-upward sequences occur within the Prairie Formation .. Near the basin center, the lowermost sequence is transitional with the underlying Winnipegosis Formation. This transition is characterized by thinly laminated carbonates that become increasingly interbedded with anhydrites of the basin-centered Ratner Member, the remainder of the sequence progresses up through halite and culminates in the halite-dominated Esterhazy potash beds. Two overlying sequences also brine upwards, however, these sequences lack the basal anhydrite and instead begin with halite and culminate in the Belle Plaine and Mountrail potash Members, respectively. -
Status of Mineral Resource Information for the Fort Berthold Indian Reservation, North Dakota
STATUS OF MINERAL RESOURCE INFORMATION FOR THE FORT BERTHOLD INDIAN RESERVATION, NORTH DAKOTA By Bradford B. Williams Mary E. Bluemle U.S. Bureau of Mines N. Dak. Geological Survey Administrative report BIA-40 1978 CONTENTS SUMMARY AND CONCLUSIONS ................................................. 1 INTRODUCTION ................................................................ 1 Area Location and Access .................................................... 1 Past Investigations .......................................................... 2 Present Study and Acknowledgments ........................................... 2 Land Status................................................................ 2 Physiography .............................................................. 3 GEOLOGY ..................................................................... 4 Stratigraphy ............................................................... 4 Subsurface .......................................................... 4 Surface ............................................................. 4 General ....................................................... 4 Bullion Creek and Sentinel Butte Formations ......................... 8 Golden Valley Formation......................................... 9 Cole Harbor Formation .......................................... 9 Structure................................................................. 10 MINERAL RESOURCES ......................................................... 11 General ................................................................. -
Mannville Group of Saskatchewan
Saskatchewan Report 223 Industry and Resources Saskatchewan Geological Survey Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan J.E. Christopher 2003 19 48 Printed under the authority of the Minister of Industry and Resources Although the Department of Industry and Resources has exercised all reasonable care in the compilation, interpretation, and production of this report, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Department of Industry and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this report. Cover: Clearwater River Valley at Contact Rapids (1.5 km south of latitude 56º45'; latitude 109º30'), Saskatchewan. View towards the north. Scarp of Middle Devonian Methy dolomite at right. Dolomite underlies the Lower Cretaceous McMurray Formation outcrops recessed in the valley walls. Photo by J.E. Christopher. Additional copies of this digital report may be obtained by contacting: Saskatchewan Industry and Resources Publications 2101 Scarth Street, 3rd floor Regina, SK S4P 3V7 (306) 787-2528 FAX: (306) 787-2527 E-mail: [email protected] Recommended Citation: Christopher, J.E. (2003): Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan; Sask. Industry and Resources, Report 223, CD-ROM. Editors: C.F. Gilboy C.T. Harper D.F. Paterson RnD Technical Production: E.H. Nickel M.E. Opseth Production Editor: C.L. Brown Saskatchewan Industry and Resources ii Report 223 Foreword This report, the first on CD to be released by the Petroleum Geology Branch, describes the geology of the Success Formation and the Mannville Group wherever these units are present in Saskatchewan. -
Bakken Production Optimization Program Executive Summary Years
Bakken Production Optimization Program EXECUTIVE SUMMARY A premier public–private partnership harnessing the best minds in North Dakota and in industry to maximize productivity of the Bakken oil play while simultaneously reducing its environmental footprint. 2 BAKKEN PRODUCTION OPTIMIZATION PROGRAM This summary of Bakken Production Optimization Program (BPOP) achievements at the end of calendar year 2015 was produced at the request of the North Dakota Industrial Commission (NDIC) and the associated Oil and Gas Research Program, which funded a portion of the work performed in this program. This summary is intended for public distribution and is intended to relay the ongoing successes of this premier public–private partnership in advancing North Dakota’s economic and environmental interests directly related to exploration and production of oil from the Bakken and Three Forks Formations. EXECUTIVE SUMMARY 1 4 PROGRAM INTRODUCTION 6 Anticipated Outcomes 8 Partnership and Members 10 OPTIMIZATION OF WELLSITE OPERATIONS 12 Flaring Reduction 14 Water Opportunities Assessment 16 TENORM Waste Disposal 18 Spills Remediation 20 THE HAWKINSON PROJECT 23 Need for the Project 24 Industry Firsts 26 Results 27 Conclusions 28 PROGRAM WORK CONTINUES 2 BAKKEN PRODUCTION OPTIMIZATION PROGRAM BAKKEN PRODUCTION OPTIMIZATION PROGRAM EXECUTIVE SUMMARY 3 In June 2013, a consortium comprising the Energy & Environmental BAKKEN Research Center (EERC), Continental Resources, Inc., and several of the largest oil producers in the state was awarded North Dakota Oil PRODUCTION -
Carboniferous Formations and Faunas of Central Montana
Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________ -
FORT BELKNAP RESERVATION List of Topics
FORT BELKNAP RESERVATION List of Topics BACKGROUND Reservation Overview Regional Geologic Overview GEOLOGIC OVERVIEW Geologic History Summary of Play Types CONVENTIONAL PLAY TYPES Play 1 - Shallow Cretaceous Biogenic Gas Play Play 2 - Northern Plains Biogenic Gas Play Plays 3,4,5 - Jurassic/Cretaceous and Mississippian Plays UNCONVENTIONAL / HYPOTHETICAL PLAY TYPES Plays 6,7 - Fractured Bakken and Cambrian Sandstone Plays REFERENCES Historical Background of the OVERVIEW (i.e. joint ventures) in contrast to procedures and regulatory minimums imposed Assiniboine and Gros Ventre Tribes at Fort Belknap by the previous 1938 Minerals Leasing Act. The 1982 Act further provides that FORT BELKNAP RESERVATION The Fort Belknap Indian Reservation was created in 1887 as the home for the individual Indian allottees may join agreements negotiated for tribal lands. The Assiniboine and Gros Ventre Tribes Assiniboine and Gros Ventre Indian Tribes. The ancestors of these tribes have section entitled Operating Regulations discusses the procedures for obtaining lived on the northern plains for several centuries. The Assiniboine were allottee participance in the negotiated agreement. recognized by Europeans as part of the great Sioux Nation and speak a Siouan Principal components for the formal corporate proposal should include the TRIBAL HEADQUARTERS: Fort Belknap Agency, Montana language. However, their name is taken from a Chippewa word referring to area(s) of interest, type of contract, elaboration of proposed agreement terms, GEOLOGIC SETTING: Williston Basin "those who cook with stones." At some point in time the Assiniboine bands points of potential negotiation, diligence commitments (i.e. drilling), bonus broke with the traditional Sioux and allied themselves with the Cree. -
Oil and Gas Potential of the Red River Formation, Southwestern North Dakota Timothy O
Oil and Gas Potential of the Red River Formation, Southwestern North Dakota Timothy O. Nesheim Introduction North Dakota has experienced commercial oil and gas production third highest for the state, a bronze medal so to speak, and is from 19 different geologic formations over the past 65 years. only eclipsed by the “gold” medal Bakken-Three Forks Formations Most of these productive formations have experienced spotlight (>1.2 billion barrels of oil) and the “silver” medal Madison Group attention from the oil and gas industry at one time or another, (Mission Canyon & Charles Formations, ~1 billion barrels of oil). and, whether for a few months or years, were considered a “hot Red River production is also regionally extensive and stretches play” to explore and develop. The unconventional Bakken-Three into northwestern South Dakota, eastern Montana, and southern Forks development is a current example of a play that brought Saskatchewan (fig. 1). oil and gas activity in the state to record levels and has sustained drilling activity even in a depressed oil and gas market. As the Summary of Red River Oil and Gas Production oil and gas industry transitions beyond the Bakken over time and The upper Red River consists of four, vertically stacked, oil- begins to spend more time evaluating the other 17 productive productive sedimentary rock layers referred to informally as the non-Bakken/Three Forks Formations, additional oil and gas plays “A” through “D” zones (fig. 2). Just over half of the Red River’s will emerge across western North Dakota. One formation that oil production has come from horizontal wells drilled within the has previously experienced “hot play” status and may be poised “B” zone of southwestern Bowman County, a prolific oil play to one day re-emerge into the spotlight of the oil and gas industry that emerged during the late 1990s and was North Dakota’s “hot is the deeply buried Red River Formation.