Depositional environments as a guide to uranium mineralization in the Chinle Formation, San Rafael Swell, Utah
Uranium deposits in the San Rafael Swell are related to sedimentary depositional environments in the Upper Triassic Chinle Formation. The sedimentary textures resulting from depositional processes operating in low-energy environments appear to have influenced uranium mineralization. The Ohinle consists of three fining-upward, fluvial-lacustrine sequences. Uranium minerals are concentrated in the lower part of the lowest sequence in areas where sediments of low-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.
|Publication Subtype||Journal Article|
|Title||Depositional environments as a guide to uranium mineralization in the Chinle Formation, San Rafael Swell, Utah|
|Series title||Journal of Research of the U.S. Geological Survey|
|Publisher||U. S. Geological Survey|
|Other Geospatial||Chinle Formation, Colorado Plateau, San Rafael Swell|
|Google Analytic Metrics||Metrics page|