Thomas Finn (Former Employee)
Science and Products
Filter Total Items: 13
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Filter Total Items: 136
Evaluation of undiscovered natural gas in the Upper Cretaceous Ferron Coal/Wasatch Plateau Total Petroleum System, Wasatch Plateau and Castle Valley, Utah
The Total Petroleum System approach was used to estimate undiscovered gas potential of the Wasatch Plateau and Castle Valley, central Utah. The Ferron Coal/Wasatch Plateau Total Petroleum System was geologically defined and subdivided into seven assessment units, six of which were formally evaluated. Geologic data considered in defining the assessment unit boundaries included thermal maturity, coa
Authors
M. E. Henry, T.M. Finn
Assessment of undiscovered oil and gas resources of the Southwestern Wyoming Province, 2002
No abstract available.
Authors
Mark Kirschbaum, Thomas M. Finn, Robert D. Hettinger, Edward A. Johnson, Ronald C. Johnson, Joyce Kibler, Paul G. Lillis, Philip H. Nelson, Laura N.R. Roberts, Stephen B. Roberts, Ronald R. Charpentier, Troy A. Cook, Robert A. Crovelli, Timothy R. Klett, Richard M. Pollastro, Christopher J. Schenk
Vitrinite reflectance data for the Greater Green River basin, southwestern Wyoming, northwestern Colorado, and northeastern Utah
The Greater Green River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 25,000 square miles in southwestern Wyoming, northwestern Colorado, and northeastern Utah (fig. 1). Important conventional oil and gas resources have been discovered and produced from reservoirs ranging in age from Cambrian through Tertiary (Law, 1996). In addi
Authors
Mark J. Pawlewicz, Thomas M. Finn
Potential for a basin-centered gas accumulation in the Albuquerque Basin, New Mexico
The potential that a basin-centered or continuous-type gas accumulation is present in the Albuquerque Basin in central New Mexico was investigated. The Albuquerque Basin is one of the many rift basins that make up the Rio Grand rift system, an area of active extension from Oligocene to recent time. The basin is significantly different from other Rocky Mountain basins that contain basin-centered ga
Authors
Ronald C. Johnson, Thomas M. Finn, Vito F. Nuccio
Potential for a basin-centered gas accumulation in the Raton Basin, Colorado and New Mexico
The Raton Basin appears to contain a significant continuous
or basin-centered gas accumulation in sandstones of the Upper Cretaceous Trinidad Sandstone and Vermejo Formation and Upper Cretaceous and Paleocene Raton Formation. The accumulation is underpressured and occurs at comparatively shallow (
Authors
Ronald C. Johnson, Thomas M. Finn
An assessment of in-place gas resources in the low-permeability basin centered gas accumulation of the Bighorn Basin, Wyoming and Montana
No abstract available.
Authors
R. C. Johnson, R. A. Crovelli, B.G. Lowell, T.M. Finn
An assessment of in-place gas in tight and near-tight reservoirs, Wind River Indian Reservation, Wyoming
No abstract available.
Authors
R. C. Johnson, R. A. Crovelli, T.M. Finn, B.G. Lowell
An assessment of in-place gas resources in low-permeability Upper Cretaceous and lower Tertiary sandstone reservoirs, Wind River Basin, Wyoming
No abstract available.
Authors
R. C. Johnson, T.M. Finn, R. A. Crovelli, R.H. Balay
Geology of Upper Cretaceous and Paleocene gas-bearing rocks, Wind River Basin, Wyoming
No abstract available.
Authors
R. C. Johnson, T.M. Finn, W. R. Keefer, R.J. Szmajter
Thermal maturity data used for the assessment of gas resources in the Wind River basin, Wyoming
No abstract available.
Authors
V. F. Nuccio, T.M. Finn, R. C. Johnson
Subsurface stratigraphic cross section of Lower and Upper Cretaceous rocks in the south eastern Wind River basin, Wyoming
No abstract available
Authors
T.M. Finn
Coalbed methane potential of the Upper Cretaceous Mesaverde and Meeteetse formations, Wind River Reservation, Wyoming
The environments of deposition of the uppermost part of the Cody Shale and the Mesaverde and Meeteetse Formations of Late Cretaceous age were studied on outcrop in the Shotgun Butte area in the north-central part of the Wind River Reservation. A shoreface sandstone occurs in the lower part of the Mesaverde Formation at all localities studied, and is directly overlain by a coaly interval. Repetitiv
Authors
R. C. Johnson, A.C. Clark, C. E. Barker, B. L. Crysdale, D. K. Higley, R.J. Szmajter, T.M. Finn
Science and Products
Filter Total Items: 13
No Result Found
Filter Total Items: 136
Evaluation of undiscovered natural gas in the Upper Cretaceous Ferron Coal/Wasatch Plateau Total Petroleum System, Wasatch Plateau and Castle Valley, Utah
The Total Petroleum System approach was used to estimate undiscovered gas potential of the Wasatch Plateau and Castle Valley, central Utah. The Ferron Coal/Wasatch Plateau Total Petroleum System was geologically defined and subdivided into seven assessment units, six of which were formally evaluated. Geologic data considered in defining the assessment unit boundaries included thermal maturity, coa
Authors
M. E. Henry, T.M. Finn
Assessment of undiscovered oil and gas resources of the Southwestern Wyoming Province, 2002
No abstract available.
Authors
Mark Kirschbaum, Thomas M. Finn, Robert D. Hettinger, Edward A. Johnson, Ronald C. Johnson, Joyce Kibler, Paul G. Lillis, Philip H. Nelson, Laura N.R. Roberts, Stephen B. Roberts, Ronald R. Charpentier, Troy A. Cook, Robert A. Crovelli, Timothy R. Klett, Richard M. Pollastro, Christopher J. Schenk
Vitrinite reflectance data for the Greater Green River basin, southwestern Wyoming, northwestern Colorado, and northeastern Utah
The Greater Green River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 25,000 square miles in southwestern Wyoming, northwestern Colorado, and northeastern Utah (fig. 1). Important conventional oil and gas resources have been discovered and produced from reservoirs ranging in age from Cambrian through Tertiary (Law, 1996). In addi
Authors
Mark J. Pawlewicz, Thomas M. Finn
Potential for a basin-centered gas accumulation in the Albuquerque Basin, New Mexico
The potential that a basin-centered or continuous-type gas accumulation is present in the Albuquerque Basin in central New Mexico was investigated. The Albuquerque Basin is one of the many rift basins that make up the Rio Grand rift system, an area of active extension from Oligocene to recent time. The basin is significantly different from other Rocky Mountain basins that contain basin-centered ga
Authors
Ronald C. Johnson, Thomas M. Finn, Vito F. Nuccio
Potential for a basin-centered gas accumulation in the Raton Basin, Colorado and New Mexico
The Raton Basin appears to contain a significant continuous
or basin-centered gas accumulation in sandstones of the Upper Cretaceous Trinidad Sandstone and Vermejo Formation and Upper Cretaceous and Paleocene Raton Formation. The accumulation is underpressured and occurs at comparatively shallow (
Authors
Ronald C. Johnson, Thomas M. Finn
An assessment of in-place gas resources in the low-permeability basin centered gas accumulation of the Bighorn Basin, Wyoming and Montana
No abstract available.
Authors
R. C. Johnson, R. A. Crovelli, B.G. Lowell, T.M. Finn
An assessment of in-place gas in tight and near-tight reservoirs, Wind River Indian Reservation, Wyoming
No abstract available.
Authors
R. C. Johnson, R. A. Crovelli, T.M. Finn, B.G. Lowell
An assessment of in-place gas resources in low-permeability Upper Cretaceous and lower Tertiary sandstone reservoirs, Wind River Basin, Wyoming
No abstract available.
Authors
R. C. Johnson, T.M. Finn, R. A. Crovelli, R.H. Balay
Geology of Upper Cretaceous and Paleocene gas-bearing rocks, Wind River Basin, Wyoming
No abstract available.
Authors
R. C. Johnson, T.M. Finn, W. R. Keefer, R.J. Szmajter
Thermal maturity data used for the assessment of gas resources in the Wind River basin, Wyoming
No abstract available.
Authors
V. F. Nuccio, T.M. Finn, R. C. Johnson
Subsurface stratigraphic cross section of Lower and Upper Cretaceous rocks in the south eastern Wind River basin, Wyoming
No abstract available
Authors
T.M. Finn
Coalbed methane potential of the Upper Cretaceous Mesaverde and Meeteetse formations, Wind River Reservation, Wyoming
The environments of deposition of the uppermost part of the Cody Shale and the Mesaverde and Meeteetse Formations of Late Cretaceous age were studied on outcrop in the Shotgun Butte area in the north-central part of the Wind River Reservation. A shoreface sandstone occurs in the lower part of the Mesaverde Formation at all localities studied, and is directly overlain by a coaly interval. Repetitiv
Authors
R. C. Johnson, A.C. Clark, C. E. Barker, B. L. Crysdale, D. K. Higley, R.J. Szmajter, T.M. Finn