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- W97439987 abstract "Uranium deposits in the San Rafael Swell are related to sedimentary depositional environments in the Triassic Chinle Formation. The sedimentary textures resulting from depositional processes operating in lower energy environments appear to have influenced uranium mineralization. The Chinle consists of three fining-upward, fluvial-lacustrine sequences. Uranium mineralization is concentrated in the lower part of the lowest sequence in areas where sediments of lower energy environments are complexly interbedded with sediments of other environments. Areas favorable for uranium exploration exist in the subsurface to the north, west, and south of the Chinle outcrop in the Swell. This determination is based on the spatial distribution of depositional environments and the pattern of Chinle deposition through time." @default.
- W97439987 created "2016-06-24" @default.
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- W97439987 date "1976-01-01" @default.
- W97439987 modified "2023-09-26" @default.
- W97439987 title "Depositional environments as a guide to uranium mineralization in the Chinle Formation, San Rafael Swell, Utah" @default.
- W97439987 doi "https://doi.org/10.3133/ofr76283" @default.
- W97439987 hasPublicationYear "1976" @default.
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