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- W216702946 abstract "Precambrian and Cambrian igneous rocks and Pennsylvanian-Permian sedimentary rocks in southwestern and southern Oklahoma are related genetically in that the former, by means of tectonism, was the dominant source material for sediments composing a substantial part of the latter. Petrological and geochemical evidence indicate that granite and rhyolite are potential sources of uranium in southwestern Oklahoma. Riebeckite-aegirine pegmatite dikes contain 38 to 108 ppM uranium. Most of the uranium anomalies in sedimentary rocks are present in association with structural features. Local reducing conditions favoring precipitation from ground water were due to seepage of hydrocarbons along faults, concentration of carbonaceous material (in one case), and deposition of cornstone (caliche). In the Vanoss Formation, the anomalous uranium content in ground water is associated with coarse-grained, arkosic facies. The structural configuration appears to have been relatively unimportant in localization of the anomalies. Some of the disseminated uranium in framework grains and clay in arkoses and subarkoses in southwestern Oklahoma was leached by ground water and transported both parallel to and across bedding (by means of fractures and capillary pressure) to local areas favorable for precipitation." @default.
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- W216702946 date "1977-06-15" @default.
- W216702946 modified "2023-09-27" @default.
- W216702946 title "Evaluation of uranium potential in selected Pennsylvanian and Permian units and igneous rocks in southwestern and southern Oklahoma. Final report" @default.
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