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- W2034697387 abstract "The mode of distribution of uranium in geological samples is closely related to the type of geochemical environment during the time of formation or alteration of a specific specimen. By high resolution micromapping of U in sediment samples from the Kaapvaal Craton, South Africa, using n-induced U-235 fission tracks in mica detectors, information is obtained about the redox potential of the hydrosphere- atmosphere system at the time of U-deposition or remobilization. Mineralogical and textural considerations as well as radioactive disequilibria in the natural U-decay series, measured by α-spectrometry, were used to identify the type of U-mobilization. The U-distribution patterns of carefully selected conglomerate samples from the Witwatersrand basin are in agreement with the assumption of a predominantly reducing Earth atmosphere at the time of basin formation some 2.6 × 109 y ago." @default.
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- W2034697387 date "1988-01-01" @default.
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- W2034697387 title "Some applications of uranium tracing in geological samples using thermal neutron induced fission" @default.
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- W2034697387 doi "https://doi.org/10.1016/1359-0189(88)90248-8" @default.
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