Petroleum potential of the Palo Duro Basin, Texas Panhandle. Report of investigations No. 123

Technical Report · Fri Jan 01 04:00:00 EST 1982

OSTI ID:6292633

Dutton, S P; Goldstein, A G; Ruppel, S C

Porous facies in Pre-Pennsylvanian, Pennsylvanian, and Permian strata are potential hydrocarbon reservoirs. Within the pre-Pennsylvanian section, shallow-marine carbonates of both Ordovician (Ellenburger Group) and Mississippian age have sufficient porosity and permeability for hydrocarbon accumulation. Three main exploration targets of Pennsylvanian and Wolfcampian age are (1) granite-wash sandstones, (2) shelf-margin carbonates, and (3) elongate-delta sandstones. Granite wash was deposited in fan deltas adjacent to fault-bounded, basement uplifts around the basin margins. Porous facies are braided-channel, fan-plain, and distal-fan deposits. Porous carbonates developed through time along the different positions of the shelf margins. Organic-rich basinal shales are juxtaposed against the porous shelf-margin facies. High-constructive, elongate-delta deposits in the southeastern part of the basin retain high porosity in bar-finder sandstones. In younger strata, dolomites in the Clear Fork and the San Andres. Porosity in these units apparently pinches out to the north. Both stratigraphic and structural traps occur in the basin. Porosity pinch-outs form the primary stratigraphic traps. Major faults are associated with the Amarillo Uplift; smaller faults have been identified in the deeper parts of the basin. The Palo Duro Basin contains source rocks of sufficient quality to generate hydrocarbons. Pennsylvanian and Wolfcampian shales contain up to 2.4 percent total organic carbon and are fair to very good source rocks. Lipid-rich organic matter occurs primarily in basinal shales. Kerogen color and vitrinite reflectance, which measure thermal maturity, indicate that temperatures were sufficiently high to begin to generate hydrocarbons from lipid-rich organic matter. Average reflectance in Pennsylvanian vitrinite is 0.52%; in Wolfcampian samples the average reflectance is 0.48%. Recent oil discoveries in the Palo Duro Basin confirm that oil was generated.

• Research Organization: Texas Univ., Austin (USA). Bureau of Economic Geology
• DOE Contract Number: AC97-80ET46615
• OSTI ID: 6292633
• Report Number(s): DOE/ET/46615-T3; ON: DE83011099
• Country of Publication: United States
• Language: English

Related Subjects

02 PETROLEUM
020200* -- Petroleum-- Reserves
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BITUMINOUS MATERIALS
CARBONACEOUS MATERIALS
CARBONATE ROCKS
CHEMISTRY
EXPLORATION
FEDERAL REGION VI
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGIC TRAPS
GEOLOGY
GRANITES
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KEROGEN
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MINERAL RESOURCES
NORTH AMERICA
OPTICAL PROPERTIES
ORGANIC MATTER
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RESOURCES
ROCKS
SANDSTONES
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SOURCE ROCKS
STRATIGRAPHY
SURFACE PROPERTIES
TECTONICS
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USA