Occurrence and geochemistry of natural gases, Piceance basin, northwestern Colorado
The Piceance basin is a hydrocarbon-rich province that has major resources of natural gas in coal beds and tight sandstone reservoirs of Cretaceous age. In general, gases from all producing intervals are of thermal origin and become isotopically heavier (/delta//sup 13/C/sub 1/ values = /minus/51.3 to -29.1 ppt) and chemically drier (C/sub 1//C/sub 1-5/ values = 0.41 to 1.00) with increasing level of thermal maturity (R/sub 0/ values = 0.45 to 2.4%) over a depth range of 1100 to 11,702 ft. Maturity increases to the south because of higher paleotemperatures. Based on chemical and isotopic composition, three types of gases can be distinguished: those generated from (1) mixed types II and III kerogens, (2) dispersed type III kerogen, and (3) coal, shown in series from chemically wettest to driest and isotopically lightest to heaviest at equivalent levels of thermal maturity. Type 1 gases are produced from marine sandstones, such as those of the Mancos B and Iles formations, and are associated with oil. Type 2 gases are in nonmarine sandstones of the Williams Fork Formation, are nonassociated at all levels of maturity, and contain large amounts of carbon dioxide (as much as 22%) derived from thermal decomposition of type III kerogen. Methane-rich type 3 gases are produced by devolatilization of humic coal and are contained in coal beds of the Cameo-Fairfield zone of the Williams Fork Formation. They have not migrated into adjacent sandstone reservoirs. Gases in immature Tertiary reservoirs are similar in chemical and isotopic composition to those of underlying reservoirs. They are interpreted to have migrated from deeper, more mature Cretaceous source rocks.
- Research Organization:
- Geological Survey, Denver, CO (USA)
- OSTI ID:
- 6128402
- Report Number(s):
- CONF-890404-
- Journal Information:
- AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States), Vol. 73:3; Conference: AAPG annual convention with DPA/EMD Divisions and SEPM, San Antonio, TX, USA, 23-26 Apr 1989
- Country of Publication:
- United States
- Language:
- English
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Geologic and hydrologic controls on coalbed methane producibility, Williams Fork Formation, Piceance Basin, Colorado
Geologic and hydrologic controls on coalbed methane producibility, Williams Fork Formation, Piceance Basin, Colorado
Related Subjects
COLORADO
NATURAL GAS DEPOSITS
GEOCHEMISTRY
ORIGIN
PICEANCE CREEK BASIN
CARBON 13
COAL SEAMS
CRETACEOUS PERIOD
KEROGEN
MATURATION
RESERVOIR ROCK
SANDSTONES
SOURCE ROCKS
TERTIARY PERIOD
BITUMINOUS MATERIALS
CARBON ISOTOPES
CARBONACEOUS MATERIALS
CENOZOIC ERA
CHEMISTRY
COAL DEPOSITS
EVEN-ODD NUCLEI
FEDERAL REGION VIII
GEOLOGIC AGES
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ISOTOPES
LIGHT NUCLEI
MATERIALS
MESOZOIC ERA
MINERAL RESOURCES
NORTH AMERICA
NUCLEI
ORGANIC MATTER
RESOURCES
ROCKS
SEDIMENTARY ROCKS
STABLE ISOTOPES
USA
030200* - Natural Gas- Reserves
Geology
& Exploration