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- W2024580076 abstract "Although uraninite is thermodynamically unstable at oxygen pressures greater than approximately 10−21 atmosphere, calculations based on the dissolution kinetics suggest that uraninite from the Witwatersrand Sequence, South Africa may have survived as a detrital mineral at oxygen pressures as high as 0.01 PAL (Present Atmospheric Level). Therefore, the deposition of the mid-Precambrian uraniferous conglomerates at Elliot Lake, Canada and Witwatersrand, South Africa does not require an essentially anoxic atmosphere as previously proposed, but may have occurred under an atmosphere containing small amounts of oxygen, consistent with photodissociation of water vapor and limited aerobic photosynthesis." @default.
- W2024580076 created "2016-06-24" @default.
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- W2024580076 date "1980-09-01" @default.
- W2024580076 modified "2023-09-25" @default.
- W2024580076 title "Origin of uraniferous conglomerates at Elliot Lake, Canada and Witwatersrand, South Africa: Implications for oxygen in the Precambrian atmosphere" @default.
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- W2024580076 doi "https://doi.org/10.1016/0301-9268(80)90056-x" @default.
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