Lewis Total Petroleum System of the Southwestern Wyoming Province, Wyoming, Colorado, and Utah Volume Title Page by Robert D

Total Page:16

File Type:pdf, Size:1020Kb

Lewis Total Petroleum System of the Southwestern Wyoming Province, Wyoming, Colorado, and Utah Volume Title Page by Robert D Chapter 9 Lewis Total Petroleum System of the Southwestern Wyoming Province, Wyoming, Colorado, and Utah Volume Title Page By Robert D. Hettinger and Laura N.R. Roberts Chapter 9 of Petroleum Systems and Geologic Assessment of Oil and Gas in the Southwestern Wyoming Province, Wyoming, Colorado, and Utah By USGS Southwestern Wyoming Province Assessment Team U.S. Geological Survey Digital Data Series DDS–69–D U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Denver, Colorado: Version 1, 2005 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 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 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. 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. Manuscript approved for publication May 10, 2005 ISBN= 0-607-99027-9 Contents Abstract ……………………………………………………………………………………… 1 Introduction …………………………………………………………………………………… 1 Acknowledgments …………………………………………………………………………… 3 Stratigraphy of Lewis Shale …………………………………………………………………… 3 Basin-Centered Gas System in the Greater Green River Basin ……………………………… 7 Lewis Total Petroleum System (503707) ……………………………………………………… 10 Hydrocarbon Source Rocks ……………………………………………………………… 10 Source Rock Maturation ………………………………………………………………… 12 Hydrocarbon Migration ………………………………………………………………… 14 Hydrocarbon Reservoir Rocks …………………………………………………………… 14 Hydrocarbon Traps and Seals …………………………………………………………… 17 Total Petroleum System Event Summary ………………………………………………… 17 Assessment Units in the Lewis Total Petroleum System ……………………………………… 19 Lewis Continuous Gas Assessment Unit (50370761) …………………………………… 20 Historical Drilling, Success Ratios, and Production ……………………………… 20 Lewis Conventional Oil and Gas Assessment Unit (50370701) …………………………… 26 Historical Drilling and Production ………………………………………………… 26 Assessment Results for the Lewis Total Petroleum System (503707) ………………………… 26 Lewis Continuous Gas Assessment Unit (50370761) …………………………………… 26 Total Assessment-Unit Area ……………………………………………………… 26 Area per Cell of Untested Cells Having Potential for Additions to Reserves in the Next 30 Years …………………………………………………………………… 30 Percentage of the Total Assessment-Unit Area that is Untested ………………… 30 Future Success Ratios for Untested Cells Having Potential for Additions to Reserves in the Next 30 Years …………………………………………………… 30 Percentage of Untested Assessment-Unit Area that has Potential for Additions to Reserves in the Next 30 Years …………………………………………………… 30 Total Recovery per Cell for Untested Cells Having Potential for Additions to Reserves in the Next 30 Years …………………………………………………… 31 Assessment Results ……………………………………………………………… 31 Lewis Conventional Oil and Gas Assessment Unit (50370701) …………………………… 31 Assessment Results ……………………………………………………………… 32 References …………………………………………………………………………………… 32 Appendix A. Basic input data for the Lewis Continuous Gas Assessment Unit (50370761) FORSPAN ASSESSMENT MODEL …………………………………………………………… 36 Appendix B. Basic input data for the Lewis Conventional Oil and Gas Assessment Unit (50370701) SEVENTH APPROXIMATION DATA FORM (NOGA, Version 5, 6-30-01) ………… 38 III Figures 1. Map showing location of the Lewis Total Petroleum System, Southwestern Wyoming Province, Greater Green River Basin ……………………………………………………… 2 2. Chart showing formations and stratigraphic relations in the Southwestern Wyoming Province …………………………………………………………………………………… 4 3. Structure contour map constructed on the base of the Lewis Shale ……………………… 5 4. Map showing overburden thickness on top of the Lewis Shale …………………………… 6 5. Geophysical log signatures of the Lewis Shale …………………………………………… 8 6. Generalized paleogeographic map of the region containing the Lewis Total Petroleum System …………………………………………………………………………………… 9 7. Map showing location of assessment units in the Lewis Total Petroleum System ……… 11 8. Map showing thermal maturity of source rock of the Lewis Total Petroleum System …… 13 9. Graph showing timing of gas generation in the Lewis Shale ……………………………… 15 10. Map showing net sandstone thickness in the Lewis Shale ……………………………… 16 11. Map showing areas of Lewis Shale that have potential for stratigraphic traps …………… 18 12. Event charts showing timing of key events in the Lewis Total Petroleum System ………… 19 13. Map showing Lewis Continuous Gas Assessment Unit …………………………………… 22 14. Tested wells in Lewis Continuous Gas Assessment Unit ………………………………… 24 15. Graphs showing distribution of estimated ultimate recoveries (EURs) for wells in the Lewis Continuous Gas Assessment Unit ………………………………………………… 25 16. Map showing Lewis Conventional Oil and Gas Assessment Unit ………………………… 27 17. Graphs showing trends through time of gas accumulation discoveries in the Lewis Conventional Oil and Gas Assessment Unit ……………………………………………… 29 Tables 1. Fields that have produced gas and(or) oil from the Lewis Total Petroleum System ………… 21 2. Reservoir characteristics for selected fields that have produced from the Lewis Continuous Gas Assessment Unit ……………………………………………………………………… 23 3. Reservoir characteristics for selected fields that have produced from the Lewis Conventional Oil and Gas Assessment Unit ………………………………………………… 28 4. Undiscovered resources in the Lewis Total Petroleum System …………………………… 30 Plate 1. Stratigraphy of the Upper Cretaceous Lewis Shale in the eastern part of the Greater Green River Basin, Colorado, and Wyoming ……………………………………………………… 35 IV Lewis Total Petroleum System of the Southwestern Wyoming Province, Wyoming, Colorado, and Utah By Robert D. Hettinger and Laura N.R. Roberts niques, and an improved understanding of the basin-centered Abstract system. As such, individual untested cells are expected to range from 20 to 200 acres in size (with a mean of 103 acres), The Lewis Total Petroleum System (TPS) within the total recovery per cell is anticipated to range from 0.02 to Southwestern Wyoming Province of Wyoming, Colorado, 15 BCFG (with a median of 0.6 BCFG), and drilling success Utah is a complex of marine strata that contains significant ratios are anticipated to range from 80 to 90 percent (with a quantities of gas sourced from dominantly Type-III kero- median of 85 percent). gen. Between 600 and 675 billion cubic feet of gas (BCFG) In contrast, most of the significant hydrocarbon accumu- and minor amounts of oil have been produced since 1974. lations in the Lewis Conventional Oil and Gas Assessment The source rock, reservoir rock, and seals are distributed Unit might have already been found. However, in the next throughout most of the Maastrichtian Lewis Shale, which was 30 years, the conventional assessment unit has the potential deposited about 71 to 68 million years ago (Ma) in the eastern to provide between about 104 and 304 BCFG, with a calcu- half of the Greater Green River Basin. Previous investigations lated mean of about 195 BCFG. This undiscovered resource is reveal that the sandstone reservoirs have a net thickness of as anticipated to be distributed throughout 8 to 31 undiscovered much as 600 feet. The sandstones were deposited in deltaic gas accumulations (with a median of 18), and the accumula- and turbidite systems, and some basin-floor sand lobes extend tion sizes are expected to range from 3 to 90 BCFG (with a across as many as 30 townships. Gas generation began about median of 8 BCFG). 62 Ma, and peak gas generation and gas migration began about 52 Ma and probably persisted until about 5 Ma when the Lewis Shale attained its maximum depth of burial. Gas gen- eration may be continuing at the present, but at a significantly Introduction reduced rate. Two assessment units comprise the Lewis TPS: these This report documents the rationale used to assess undis- are the Lewis Continuous Gas Assessment Unit (50370761) covered hydrocarbon resources within the Lewis Total Petro- and the Lewis Conventional Oil and Gas Assessment Unit leum System (TPS) (503707), which is complete with source (50370701). The former encompasses approximately 3,310,000 rock, reservoir rock, and seals. The assessment was made acres and defines deeper basin regions that are characterized by using techniques and methodology described in Chapters an overpressured, gas-saturated basin-centered accumulation. 18–23 of this CD–ROM and is based on oil and gas field infor- The latter encompasses approximately 3,820,000 acres and mation provided by NRG Associates (2001), well history and defines shallower basin regions where gas accumulations are production data by the IHS Energy Group (2001), and critical within conventional-style traps. The assessment of both units geologic input described in this report. Included are discus- is based on stratigraphic and structural information and his- sions on (1) stratigraphy of the Lewis Shale, (2) the Lewis torical production data. Assessment results report hydrocarbon TPS, (3) source rock maturation, (4) hydrocarbon migration, resources that have the potential to be produced in the next 30 (5)
Recommended publications
  • 2020 Annual Report
    ANNUAL REPORT 2 MISSION + BOARD MEMBERS AND STAFF 7 BOARD PROJECTS 3 BUDGET BREAKDOWN + BLOCK GRANTS 8–9 MEDIA, MARKETING & PUBLIC RELATIONS 4 EVENT GRANTS + EVENT RECRUITMENT 10 TRAVEL IMPACT STUDIES 5 COMMITTEES & BOARDS + STRATEGIC PLAN 11 2019 TRAVEL IMPACTS 6 R.E.A.C.H. AWARDS + TOURISM AMBASSADORS EXPLOREWY.COM OUR BOARD MEMBERS & STAFF MISSION: FRONT ROW BACK ROW NOT PICTURED LINDA MCGOVERN MARK LYON JANET HARTFORD TO ENHANCE THE Board Member Board Vice-Chair Board Member BRIDGET RENTERIA ERIKA LEE-KOSHAR DOMINIC WOLF ECONOMYOF Board Chair Board Member Board Member SWEETWATER JENISSA MEREDITH KIM STRID LUCY DIGGINS-WOLD COUNTY BY Executive Director Board Member Tour Guide ATTRACTING AND ANGELICA WOOD DEVON BRUBAKER GRACE BANKS RETAINING Board Member Board Treasurer Visitor Assistant STACY COLVIN GREG BAILEY Board Secretary VISITORS. Board Member The lodging tax was originally approved by Sweetwater County voters in 1991 at 2%. Sweetwater CHEZNEY GOGLIO County voters approved increasing the lodging tax to Marketing Assistant 3% in 2014 and 4% in 2018 with over 80% support. LOCATION, LOCATION, LOCATION. In April 2020, Sweetwater County Travel and Tourism relocated their office to 1641 Elk Street and opened the “Explore Rock Springs and Green River, WY Visitor Center.” Elk Street (Hwy 191) is the perfect location to offer information and encourage travelers to spend more time in Rock Springs and Green River as they travel to and from Yellowstone and Grand Teton National Parks. 2 BUDGET LODGING TAX BREAKDOWN COLLECTION FISCAL YEAR TOTAL
    [Show full text]
  • 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 ................
    [Show full text]
  • 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 .
    [Show full text]
  • 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 ...........................................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 1176 Miles from Omaha to Sacramento O N T R a C K S
    RAILWAY AT DALE CREEK BRIDGE, WYOMING 69 18 Y, MA R D E E A E L N N Y E H E C E H Promontory Summit, Utah T Golden Spike Ceremony Ohmaha, NE NEWDRAFT Sacramento, CA 1869 - May 10th. - 1869 YoRK ! DRAFT GREAT EVENT ! RAIL ROAD FROM THE ATLANTIC TO THE PACIFIC GRAND OPENING t r a i n "dining saloon" ’ E a t i n s t y l e R A I L S w h i l e t r a v e l i n g T I C K E T S THE GREAT TRANS-CONTINENTAL ALL-RAIL ROUTE KID the tracks. -Business Men- - $ 1 1 1 FOR FIRST CLASS T a k e a d va n d a g e FACT 4 8 p e o p l e t o a c a r - HEATED CAR o f n e w ly o p e n e d - COMFORTABLE BEDS a s i a n m a r k e t s v i a fastest way to go coast to coast - no more wagon trains TRAINS TRAVELED c a l i f o r n i a - F O R T H I R d Almost M e n u $ 4 0 MPH CLASS TICKETS in 1869 - W O O D E N B E N C H E S - -Settlers!- Fried Salmon Steak ............................ 35c Boiled Ox Tongue with Tomato Sauce... 35c O N L Y A F E W I t ' s y o u r 1176 Miles from Omaha to Sacramento Pickled Lam’s Tongue..........................
    [Show full text]
  • CD-C FEIS Chapter 3. Affected Environment
    3. AFFECTED ENVIRONMENT 3.0 INTRODUCTION Chapter 3 describes the condition of the human and natural environment in the CD-C project area. Under NEPA, the human environment is the natural and physical environment and the relationship of people to that environment. The affected environment for individual resources was delineated based on the area of potential direct and indirect environmental impacts for the project and associated cumulative effects area. The environmental baseline information summarized in this chapter was obtained from the review of published sources, unpublished data, communication with government agencies, and review of field studies of the area. The level of information provided in this chapter is commensurate with the potential impacts to the resource described. PHYSICAL ENVIRONMENT 3.1 GEOLOGY 3.1.1 Physiography The project area straddles the Continental Divide and lies within the Great Divide and Washakie Basins, subsidiary basins of the Greater Green River Basin of south-central Wyoming (Map 3.1-1). Important natural landmarks in the area and their corresponding elevations are shown in Table 3.1-1. Table 3.1-1. Important natural landmarks in the CD-C project area (north to south) Landmark Location Elevation (feet) Lost Creek Butte NW ¼ Section 24, T23N:R95W 6,745 Stratton Knoll N ½ Section 28, T23N:R91W 6,879 Ruby Knolls Sections 26 and 27, T22N:R92W 7,165 Windy Hill (mesa) Sections 1–5, 7–12, and 18, T21N:R91W 7,125 Latham Point SW ¼ Section 32, T21N:R92W 7,235 Tipton Buttes NE ¼ Section 27, T20N:R96W 7,094 Cow/Horse Butte SE ¼ NE ¼ Section 5, T19N:R91W 7,170 High Point SW ¼ SW ¼ SE ¼ Section 17, T19N:R92W 7,321 Sugarloaf SE ¼ SW ¼ Section 5, T18N:R92W 7,088 Pine Butte Center of NW ¼ Section 10, T17N:R92W 6,808 Baldy Butte SW ¼ NW ¼ SW ¼ Section 12, T17N:R92W 6,920 North Flat Top SW ¼ Section 35 T15N:R93W and NW ¼ Section 2, T14N:R93W 7,822 East Flat Top Center of the E ½ Section 18, T14N:R92W 7,560 Continental Divide-Creston Natural Gas Development Project Final EIS April 2016 3-1 CHAPTER 3—AFFECTED ENVIRONMENT—GEOLOGY Map 3.1-1.
    [Show full text]
  • Sequence Stratigraphy of the Lower Pierre Shale in Southern
    SEQUENCE STRATIGRAPHY OF THE LOWER PIERRE SHALE IN SOUTHERN POWDER RIVER BASIN, WYOMING, USA By Armagan Kaykun 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: ____________________________ Armagan Kaykun Signed: ____________________________ Dr. Stephen A. Sonnenberg Thesis Advisor Golden, Colorado Date _____________ Signed: ____________________________ Dr. Paul M. Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Powder River Basin is one of the biggest interior sedimentary basins in the Rocky Mountain region. The Upper Cretaceous section of the southern Powder River Basin includes the Niobrara Formation, which is one of the most significant source rocks of the Western Interior Cretaceous Seaway, and it is overlain by lower Pierre Shale which consists mostly of progradational shale sequences and two productive sandstone members encased in these shales. In the southern Powder River Basin, the lower Pierre Shale is made up of eight members. These members are progradational highstand deposits of the Gammon Ferruginous Member; lowstand prograding wedge deposits consisting of the Shannon Sandstone, the Unnamed Member, and the Sussex Sandstone; transgressional Ardmore Pedro Bentonite Beds and Sharon Springs members; and highstand deposits of the Mitten Black Shale and Red Bird Silty members. The Shannon and Sussex sandstone members are known targets for oil production. The Sharon Springs Member of the lower Pierre shale has relatively high organic carbon content. Therefore, determining its continuity throughout the study area and its source rock potential was one of the main focuses of this study in addition to building the sequence stratigraphic framework for the lower Pierre Shale interval.
    [Show full text]
  • Red-Desert-Driving-Tour-Map
    to the northeast and also marks a crossing of the panorama of desert, buttes, and wild lands. A short South Pass Historical Marker the vistas you see here are remarkably similar to Hikers can remain along the rim or drop down into Honeycomb Buttes historic freight and stage road used to haul supplies walk south reveals the mysterious Pinnacles. The South Pass area of the Red Desert has been a those viewed by thousands of travelers in the past. the basin. Keep an eye out for fossils, raptors, and The Honeycomb Buttes Wilderness Study Area is to South Pass City. See map for recommended hiking human migration pathway for millennia. The crest A side road from the county road will take you to bobcat tracks. one of the most mesmerizing and difficult-to-access access roads for hiking in this wilderness study area. The Jack Morrow Hills several historical markers memorializing South Pass of the Rocky Mountains flattens out onto high-el- landscapes in the Northern Red Desert. These The Great Divide Basin The Jack Morrow Hills, named for a 19th-century evation steppes, allowing easy passage across and the historic trails. Oregon Buttes badlands are made of colorful sedimentary rock crook and homesteader, run north-south between the Continental Divide. Native Americans and their The Oregon Buttes, another wilderness study layers shed from the rising Wind River Mountains As you drive through this central section of the the Oregon Buttes and Steamboat Mountain and ancestors crossed Indian Gap to the south and Whitehorse Creek Overlook area, stand proudly along the Continental Divide, millions of years ago.
    [Show full text]
  • Geology of the Fox Hills Formation (Late Cretaceous
    GEOLOGY OF THE FOX HILLS FORMATION (LATE CRETACEOUS) IN THE WILLISTON BASIN OF NORTH DAKOTA, WITH REFERENCE TO URANIUM POTENTIAL by A. M. CVANCARA UNNERSITY OF NORTIl DAKOTA DEPARTMENT OF GEOLOGY GRAND FORKS, NORTII DAKOTA 58202 REPORT OF INVESTIGATION NO. 5S NORTH DAKOTA GEOLOGICAL SURVEY E. A. Noble, State Geologist 1976 PREPARED FOR mE U.S. ENERGY RESEARCH AND DEVELOPMENT ADMINISTRATION GRAND JUNCTION OFFICE UNDER CONTRACT NO. AT(05-1)-1633 G1O-1633-1 CONTENTS ABSTRACT ~ag~ INTRODUCTION . 1 ACKNOWLEDGMENTS .... 1 MATERIALS AND METHODS 2 STRATIGRAPHY ......................... .. .. 2 Definition and relationship to other rock units .. 2 Distribution . .. 3 Lithology and sedimentary structures .. 3 Persistence of lithologic units ... .. 7 Contacts .. ... .. .. ., 7 Thickness . .. ... .. 8 STRUcrURE ... 8 PALEONTOLOGY . 9 Fossil groups . 9 Occurrence of fossils · ..... , 9 AGE AND CORRELATION 10 DEPOSITIONAL ENVIRONMENTS .............................. 10 URANIUM POTENTIAL . · 12 General . .. ., 12 Fox Hills Formation . 13 REFERENCES . · 14 ILLUSTRATIONS Figure Page 1. Fox Hills and adjacent Formations in North Dakota (modified from Carlson, 1973) . 4 2. Schematic stratigraphic column of Fox Hills Formation in North Dakota (modified slightly from Erickson, 1974, p. 144). The Linton Member was named by Klett and Erickson (1976). 5 Plate 1. Northwest-southeast cross section (Dunn to Sioux Counties) of Fox Hills Formation in southwestern North Dakota . (in pocket) 2. Southwest-northeast cross section (Bowman to Pierce Counties) of Fox Hills Formation in western North Dakota (in pocket) 3. Southwest-northeast cross section (Adams to Burleigh Counties) of Fox Hills Formation in southwestern North Dakota (in pocket) 4. Isopach map of Fox Hills Formation in North Dakota (in pocket) ABSTRACT model is followed for the deposition of Fox Hills sediments.
    [Show full text]
  • Analysis of Low-Permeability Gas Sands Suitable for Future Research Programs
    Title Analysis of Low-Permeability Gas Sands Suitable for Future Research Programs Contractor Bureau of Economic Geology, The University of Texas at Austin, GRI Contract No. GRI-BEG-SC-112-82 Technical Past and current research on tight gas sands has focused primarily Perspective on lenticular sands. Blanket-geometry .sands were deposited by different depositional systems than lenticular sands; hence they ha ve different external and internal reservoir geometries and require different techniques to find, to develop, and to produce the contained gas. To assure that research on selected tight gas sand reservoirs would be applicable to other reservoirs, a survey was conducted with emphasis on clastic depositional systems and the expected transferability of results between stratigraphic units. Five stratigraphic units were selected for additional study, on the basis of this survey, and data collection for expanded study of these units was initiated during this contract period. Results A work plan was prepared for analysis of five stratigraphic units. The plan includes preparation of geologic cross sections and maps, review of producti ve areas, analysis of resources, and documentation of results. The units being studied are the Travis Peak Formation, the Corcoran and Cozzette Sandstones, the Mancos "B" interval of the Mancos Shale, the upper Almond Formation, and the Frontier Formation. Data acquired include 208 well logs in Colorado and 372 well logs in Wyoming; 170 well logs from Bureau files have been identified for the Travis Peak. Wells suitable for use on cross sections have been identified for the Travis Peak and Corcoran/Cozzette, and three cross sections have been prepared in the latter trend.
    [Show full text]
  • Greater Jeffersontown Historical Society Newsletter
    GREATER JEFFERSONTOWN HISTORICAL SOCIETY NEWSLETTER August 2018 Vol. 16 Number 4 August Meeting -- 12:30 P.M., Monday, August 6, 2018. We will continue to meet during the day at 12:30 P.M. in the Jeffersontown Library, 10635 Watterson Trail. The Greater Jeffersontown Historical Society meetings are held on the first Monday of the even numbered months of the year. Everyone is encouraged to attend to help guide and grow the Society. August Meeting Kentucky’s Native History - Persistent Myths and Stereotypes. The many cultural contributions Native Americans have made throughout Kentucky’s history, as well as the impact of lingering stereotypes. The program will be presented by Tressa Brown, who received her B.A. in Biology and Anthropology at Transylvania University and her M.A. in Anthropology from Arizona State University. She is currently the coordinator for the Kentucky Native American Heritage Commission and the Kentucky African American Heritage Commission. She has worked for the past 25 years providing Native American educational programming for schools and the public, both in her current position as well as in her previous position as Curator at the Salato Wildlife Education Center. Her primary focus has been to identify the stereotypes and myths about Native Americans in general and Kentucky’s Native people in particular. Her position at KHC is to provide accurate information to educators and the public about the diversity of Native cultures as well as the issues affecting Native people in contemporary society. GJHS on Facebook Thanks to Anne Bader GJHS is now on Facebook and Facebook .com. Please look at all she has put on it.
    [Show full text]