Petroleum source rock potential and thermal maturity: Palo Duro Basin, Texas

dc.coverage.box-103.0594, -100, 36.5, 33.3667
dc.creatorDutton, S. P.
dc.date.accessioned2019-10-28T18:41:39Z
dc.date.available2019-10-28T18:41:39Z
dc.date.issued1980
dc.descriptionBureau 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.abstractSamples 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.departmentBureau of Economic Geology
dc.description.departmentUT Libraries
dc.format.dimensionsiv, 48 p. : ill., maps ; 28 cm.
dc.identifierGC8010
dc.identifier.citationDutton, 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.urihttps://hdl.handle.net/2152/78013
dc.identifier.urihttp://dx.doi.org/10.26153/tsw/5102
dc.publisherUniversity of Texas at Austin. Bureau of Economic Geology
dc.relation.ispartofVirtual Landscapes of Texas
dc.relation.ispartofGeological Circulars
dc.relation.ispartofseriesGeological Circular (University of Texas at Austin. Bureau of Economic Geology), 80-10
dc.rights.restrictionOpen
dc.subjectGeology -- Texas -- Palo Duro Basin
dc.subjectGeology -- Stratigraphic -- Pennsylvanian
dc.subjectGeology -- Stratigraphic -- Permian
dc.subjectPetroleum -- Geology -- Texas -- Palo Duro Basin
dc.titlePetroleum source rock potential and thermal maturity: Palo Duro Basin, Texas
dc.typeOther

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