Petroleum source rock potential and thermal maturity: Palo Duro Basin, Texas
dc.coverage.box | -103.0594, -100, 36.5, 33.3667 | |
dc.creator | Dutton, S. P. | |
dc.date.accessioned | 2019-10-28T18:41:39Z | |
dc.date.available | 2019-10-28T18:41:39Z | |
dc.date.issued | 1980 | |
dc.description | Bureau Publication GC8010 - to purchase a print copy please go to: https://store.beg.utexas.edu/geologic-circulars/454-gc8010.html Contract no. DE-AC97-79ET44614 | |
dc.description.abstract | Samples collected from 20 geographically widespread wells in the sparsely drilled Palo Duro Basin were analyzed for total organic carbon content (TOC). Highest values of TOC, up to 6.9 percent, occur in Upper Permian San Andres dolomite in the southern part of the basin. Pennsylvanian and Lower Permian (Wolfcampian) basinal shales contain up to 2.4 percent TOC and are fair to very good source rocks. Kerogen color and vitrinite reflectance, which indicate maximum paleotemperatures, were analyzed in all samples containing greater than 0.5 percent TOC. Pennsylvanian and Wolfcampian kerogen is yellow orange to orange, an indication that temperatures were sufficiently high to begin to generate hydrocarbons from lipid-rich organic material. Palo Duro Basin samples have a broad range of vitrinite reflectance values, but populations with the lowest reflectance probably indicate the true temperatures that were reached in the basin. Average reflectance in representative Pennsylvanian vitrinite is 0.52 percent; in Wolfcampian samples the average reflectance is 0.48 percent. These values are consistent with kerogen color and suggest that basinal source rocks may have begun to generate hydrocarbons. | |
dc.description.department | Bureau of Economic Geology | |
dc.description.department | UT Libraries | |
dc.format.dimensions | iv, 48 p. : ill., maps ; 28 cm. | |
dc.identifier | GC8010 | |
dc.identifier.citation | Dutton, S. P., 1980, Petroleum Source Rock Potential and Thermal Maturity, Palo Duro Basin, Texas: The University of Texas at Austin, Bureau of Economic Geology Geological Circular 80-10, 48 p. | en_US |
dc.identifier.uri | https://hdl.handle.net/2152/78013 | |
dc.identifier.uri | http://dx.doi.org/10.26153/tsw/5102 | |
dc.publisher | University of Texas at Austin. Bureau of Economic Geology | |
dc.relation.ispartof | Virtual Landscapes of Texas | |
dc.relation.ispartof | Geological Circulars | |
dc.relation.ispartofseries | Geological Circular (University of Texas at Austin. Bureau of Economic Geology), 80-10 | |
dc.rights.restriction | Open | |
dc.subject | Geology -- Texas -- Palo Duro Basin | |
dc.subject | Geology -- Stratigraphic -- Pennsylvanian | |
dc.subject | Geology -- Stratigraphic -- Permian | |
dc.subject | Petroleum -- Geology -- Texas -- Palo Duro Basin | |
dc.title | Petroleum source rock potential and thermal maturity: Palo Duro Basin, Texas | |
dc.type | Other |
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