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4 edition of Thermal maturity data used for the assessment of gas resources in Wind River Basin, Wyoming found in the catalog.

Thermal maturity data used for the assessment of gas resources in Wind River Basin, Wyoming

Thermal maturity data used for the assessment of gas resources in Wind River Basin, Wyoming

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Published by U.S. Dept. of the Interior, U.S. Geological Survey in [Reston, Va.] .
Written in English

    Subjects:
  • Natural gas -- Wyoming -- Wind River Basin,
  • Geology, Stratigraphic -- Cretaceous

  • Edition Notes

    Statementby Vito F. Nuccio, Thomas M. Finn, and Ronald C. Johnson
    SeriesOpen-File Report -- 96-064, U.S. Geological Survey open-file report -- 96-064
    ContributionsFinn, Thomas M, Johnson, Ronald Carl, 1950-, Geological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Pagination1 v
    ID Numbers
    Open LibraryOL13620776M
    OCLC/WorldCa37184327

    Spatial variability of coalbed natural gas Produced Water Quality, Powder river Basin, Wyoming: implications for Future Development Wyoming State Geological Survey Report of Investigations No. 64 Scott A. Quillinan1,2,3 and Carol D. Frost3 1Wyoming State Geological Survey, Laramie, Wyoming


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Thermal maturity data used for the assessment of gas resources in Wind River Basin, Wyoming Download PDF EPUB FB2

Thermal Maturity Data Used for the Assessment of Gas Resources in the Wind River Basin, Wyoming: Usgs Open-File Report [V. Nuccio, T. Finn, R. Johnson] on *FREE* shipping on qualifying offers.

The United States Geological Survey (USGS) is a scientific organization created inand is part of the U.S. : T. Finn. Thermal maturity data used for the assessment of gas resources in Wind River Basin, Wyoming [microform] / by Vito F.

Nuccio, Thomas M. Finn, and Ronald C. Johnson U.S. Dept. of the Interior, U.S. Geological Survey [Reston, Va.] Thermal maturity data used for the assessment of gas resources in Wind River Basin, Wyoming. THERMAL MATURITY DATA USED FOR THE ASSESSMENT OF GAS RESOURCES IN THE WIND RIVER BASIN, WYOMING by Vito F.

Nuccio, Thomas M. Finn, and Ronald C. Johnson INTRODUCTION The Wind River Basin, Wyoming (fig. 1), contains significant resources of natural gas in low-permeability (tight) sandstone reservoirs.

From through the by: 5. Wyoming, Petroleum Systems and Geologic Assessment of Oil and Gas Resources in the Wind River Basin Province, Wyoming: U.S. Geological Survey Digital Data Series DDS–69–J, chap.

4, 96 p., CD– by: 2. Assessment of continuous oil and gas resources in the Niobrara interval of the Cody Shale, Wind River Basin Province, Wyoming, Using a geology-based assessment methodology, the U.S.

Geological Survey estimated means of million barrels of oil and trillion cubic feet of gas in the Niobrara interval of the Cody Shale in the Wind River Basin.

The thermal maturity of source rocks is greatest in the deep northern and central parts of the province and decreases to the south and east toward the basin margins.

The results of the modeling indicate that, in the deepest areas, (1) peak petroleum generation from Cretaceous rocks occurred from Late Cretaceous through middle Eocene time. National Assessment of Oil and Gas Project - Wind River Basin Province () Assessment Units Quarter-Mile Cells Metadata Updated: Janu Cell maps for each oil and gas assessment unit were created by the USGS to illustrate the degree of exploration, type of production, and distribution of production in an assessment unit or h Year: Based on thermal maturity values and geothermal gradients, the Bighorn Basin is relatively "cool" compared to other Rocky Mountain foreland basins.

Even in the deepest part of the basin, at reconstructed burial depths in excess of 20, ft (6, m), Cretaceous source rocks are still within the window for liquid hydrocarbon by: 7. Thermal maturity history and petroleum generation modelling for the Lower Cretaceous Abu Gabra Formation in the Fula Sub-basin, Muglad Basin, Sudan Wind River Basin Province Assessment Team.

Zhao et al. () used a maturity index derived from Archie equation and related this index to gas to oil ratio; Kuhn et al. () used basin/petroleum system. Burial History, Thermal Maturity, and Oil and Gas Generation History of Petroleum Systems—Wind River Basin Province Figure.

Generalized stratigraphic chart of Pennsylvanian (part) through lower Tertiary (part) rocks in Wind River Basin Province, central Wyoming.

Time spans and thicknesses not shown in correct by: 2. Petroleum Systems and Geologic Assessment of Oil and Gas in the Wind River Basin Province, Wyoming. Resources of the Wind River Basin Province, Wyoming, Compiled by USGS Wind River Basin Province Assessment Team.

Chapter 2. Tabular Data and Graphical Images in Support of the U.S. Geological Survey National Oil and Gas Assessment — The Wind River Basin Province. By T.R. Klett and P.A. Chapter 3. Geologic Assessment of. @article{osti_, title = {Relationships of source rock, thermal maturity, and overpressuring to gas generation and occurrence in low-permeability upper Cretaceous and lower Tertiary rocks, Greater Green River basin, Wyoming, Colorado, Utah}, author = {Law, B.E.}, abstractNote = {Most hydrocarbon production from low-permeability Upper Cretaceous and.

Thermal maturity data used for the assessment of gas resources in the Wind River basin, Wyoming; ; OFR; ; Nuccio, V. F.; Finn, T. M.; Johnson, R. Year Published: Genesis and residence times of soil and weathering profiles on residual and transported parent materials in the Pine Mountain area of west-central Georgia.

Maps showing thermal maturity of Upper Cretaceous marine shales in the Wind River Basin, Wyoming. The Wind River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 7, square miles in central Wyoming.

The basin is bounded by the Washakie Range, Owl Creek, and southern Bighorn. To examine the state of hydrocarbons and water in the Wind River Basin of Wyoming, the following data types are compiled and presented at the basin scale: fluid type, pressure, and temperature from drillstem tests; watersalinity and cumulative hydrocarbon production from oil and gas wells; vitrinite reflectance data; and sonic well logs.

The spatial distribution of produced. 1  Assessment of Undiscovered Oil and Gas in the Wind River Basin Province, Wyoming Table 1.

Rock-Eval and total organic carbon data for the Wind River Basin, central Wyoming.—Continued. Map number in column 1 refers to location shown Author: Thomas M. Finn. Reservoir characterization of the Mississippian Madison Formation, Wind River Basin, Wyoming Article (PDF Available) in AAPG Bulletin 88(4) April with Reads How we measure 'reads'.

An Assessment of In-Place Gas Resources in Low-n. ~ ~ ' T ~ Limits on using variations in thermal maturity to define the '- ;nn 17 Wind River Basin, Wyoming.

4 Flgure 3: Map showm15 10cauons or oit ana gas ne10s in Lilt. Geothermal Uses. Examples in Wyoming—The historic use of geothermal resources in Wyoming is limited to "direct use" native peoples used the warm springs for medicinal and spiritual reasons. The springs subsequently provided similar resources to settlers during the great westward expansion of the s.

tions—three basin-centered gas, one oil, and two coalbed gas—are interpreted to be present in the basin. These AUs, as defined by their limits, have little or no drillstem tests and little production data, so geologic analogs from similar AUs in the Wind River Basin and Southwestern Wyoming Provinces were used to infer production potentials.

Coal Bed and Conventional Reservoirs, Wind River Basin, Wyoming RONALD C. JOHNSON and DUDLEY D. RICE 1 ABSTRACT Variations in the chemical and isotopic compositions (0~3C~ or methane) of gases from the Wind River Basin, central Wyoming, were studied in order to better understand the origins of the gases.

Oil and Gas and Other Resources of the Wind River Basin, Wyoming; Special Symposium, Pages An Empirical Correlation Between Coal Bed Gas with Rock-Eval Pyrolysis and 13 C NMR Results, Cretaceous Mesaverde and Meeteetse Formations, Wind River Basin, Wyoming.

Barker, T. Bartke, P. Hatcher, T. Daws. Abstract. The Greater Green River Basin (GGRB) is a 21, square mile basin located in Southwestern Basin was formed during the Cretaceous period sourced by underlying Permian and Cretaceous deposits. The GGRB is host to many anticlines created during the Laramide Orogeny trapping many of its hydrocarbon resources.

It is bounded by the Rawlins Uplift. Summary The Wind River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 7, square miles in central Wyoming (fig. The basin is bounded by the Washakie Range and Owl Creek and southern Bighorn Mountains on the north, the Casper arch on the east.

The purpose of the U.S. Geological Survey's (USGS) National Oil and Gas Assessment is to develop geologically based hypotheses regarding the potential for additions to oil and gas reserves in priority areas of the United States. The U.S. Geological Survey (USGS) recently completed an assessment of the undiscovered oil and gas potential of the Wind River Basin.

Abstract. This report describes the geothermal resources of the Southern Powder River Basin. The report contains a discussion of the hydrology as it relates to the movement of heated water, a description and interpretation of the thermal regime, and four maps: a generalized geological map, a structure contour map, a thermal gradient contour map, and a ground water.

The abundance of new borehole data from recent coal bed natural gas development in the Powder River Basin was utilized by the U.S.

Geological Survey for the most comprehensive evaluation to date of coal resources and reserves in the Northern Wyoming Powder River Basin assessment : David C. Scott. Influence of Source Rock Type, Thermal Maturity, and Migration on Composition and Distribution of Natural Gases, Uinta Basin, Utah.

Dudley D. Rice, Thomas D. Fouch, Ronald C. Johnson. Abstract. Based on chemical and isotopic composition, two groups of thermogenic natural gas can be distinguished in the Uinta Basin.

Distribution of d 34 S values by boiling point for fractions of Bighorn Basin oils of different thermal maturities and TSR alteration.

Dashed lines indicate the whole oil d 34 S values, and. The boundaries of the assessment units were determined by the Wind River Assessment Team, and were drawn on the basis of geologic characteristics and conditions favorable for hydrocarbon generation and accumulation-such as source, reservoir, and seal rocks; burial, thermal, and migration histories; and trapping mechanisms-that combine to.

@article{osti_, title = {Maturation history and thermal evolution of Cretaceous source rocks of Bighorn basin, Wyoming and Montana}, author = {Hagen, E.S. and Surdam, R.C.}, abstractNote = {The Laramide basins of the Rocky Mountain region are deep asymmetric structural depressions containing thick sequences of Upper Cretaceous and Tertiary.

Keywords: basin comparison; coalbed gas; coal rank, gas content, hydrology, coalbed methane production, resources, and exploration fairways; Greater Green River, Piceance, Powder River, and Raton Basins; tectonic and stratigraphic setting: thermal maturity, Upper Cretaceous-lower Tertiary coal bedsPrice: $ This contrasts with the Wind River Basin to the south where the majority of the basin-centered gas accumulation appears to be overpressured.

Present-day temperatures and levels of thermal maturity appear to have been somewhat higher at the onset of overpressuring in the Bighorn Basin than in the Wind River by: 3.

Thermal-maturity data-indicators of maximum burial temperatures-provide important constraints both on basin evolution and on terrane amalgamation.

To help elucidate these relations, and to provide constraints for hydrocarbon assessments, the U.S. Geological survey (USGS) has compilied thermal-maturity data from Alaska for many decades. Large gas resources occur in low-permeability Upper Cretaceous and Lower Tertiary reservoirs in the Greater Green River basin of Wyoming, Colorado, and Utah.

Most of the gas-bearing reservoirs are overpressured, beginning at depths offt ( m). The reservoirs are typically. Thermal history of the Krishna-Godavari basin, India: Constraints from apatite fission track thermochronology and organic maturity data Article in Journal of Asian Earth Sciences The fundamental geologic unit used in the National Oil and Gas Assessment was the play, which is defined as a set of known or postulated oil and or gas accumulations sharing similar geologic, geographic, and temporal properties, such as source rock, migration pathways, timing, trapping mechanism, and hydrocarbon type.

The geographic limit of each play was defined. Structural Divisions of the Bighorn Mountains and Western Powder River Basin. Gary Bible. Blockchain in Industry - How the Oil and Gas Industry is Utilizing these Emerging Technologies.

M.A. Bingle-Davis. Mineralogical and Geochemical Properties of the Cretaceous Mowry Shale in the Wind River Basin, Wyoming Near the Casper Arch.Stratigraphic Model for Lower and Upper Cretaceous Strata of the East Texas Basin – Constraints From Core, Wireline-Log, and 2-D Seismic Data P. Soto-Kerans A Predictive Model of Dolomitization and Its Control on Reservoir Quality and Seismic Attributes in the Viola Formation, Morrison NE Field, Clark County, Kansas.“Longitudinal Changes in Potential Toxicity of Coalbed Natural Gas Produced Water Along Beaver Creek in the Powder River Basin, Wyoming.” M.S.

Department of Zoology and Physiology, December 21_ Kirkpatrick, Amber, Krista Pearson, and James Bauder.