2008
DOI: 10.1306/04020806015
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Modeling of gas generation from the Cameo coal zone in the Piceance Basin, Colorado

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Cited by 40 publications
(28 citation statements)
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References 36 publications
(33 reference statements)
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“…In coal, the lower boundary of the thermogenic gas window corresponds approximately with a vitrinite reflectance (R o ) of 0.8% ( Jüntgen and Klein, 1975). Closed system pyrolysis experiments suggest that coal can generate 4 to 10 times more methane than can be retained in coal matrix (Zhang et al, 2008). The excess gas will be expelled through adjacent strata if coal is poorly confined, will migrate along bedding if coal is well confined, and will contribute to overpressuring and cleating if the coal is confined and has low permeability.…”
Section: Geothermicsmentioning
confidence: 99%
“…In coal, the lower boundary of the thermogenic gas window corresponds approximately with a vitrinite reflectance (R o ) of 0.8% ( Jüntgen and Klein, 1975). Closed system pyrolysis experiments suggest that coal can generate 4 to 10 times more methane than can be retained in coal matrix (Zhang et al, 2008). The excess gas will be expelled through adjacent strata if coal is poorly confined, will migrate along bedding if coal is well confined, and will contribute to overpressuring and cleating if the coal is confined and has low permeability.…”
Section: Geothermicsmentioning
confidence: 99%
“…Coal can generate 3 to 20 times more thermogenic gas than can be retained by adsorption, which can lead to significant updip migration and expulsion (Zhang et al, 2008), and the very low permeability of the strata bounding coal seams in the Pottsville Formation probably favored updip migration within coal over direct expulsion. However, the adsorption capacity of coal increases during regional uplift and cooling, and so it is widely thought that coal can be substantially undersaturated with thermogenic gas if not augmented by hydrocarbon migration or late-stage bacterial methanogenesis (Yang and Saunders, 1985;Scott, et al, 1994).…”
Section: Burial History and Gas Generationmentioning
confidence: 99%
“…The Cameo coal zone varies in thickness from 400 to 500 feet and is comprised of interbedded sandstones, shales, and coals. The Cameo zone is thought to be a source for the Williams Fork gas (Zhang et al 2008). In the basin center of this study area, Williams Fork gas saturations can extend over 1,700 feet above the Rollins Sandstone.…”
Section: Production Profiling -Challenging Factorsmentioning
confidence: 99%