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Scanning-electron-microscope investigation of paragenesis of uranium deposits, Mount Taylor and elsewhere, Grants Mineral Belt

Conference · · Mem. - N.M. Bur. Mines Miner. Resour.; (United States)
OSTI ID:6135230
 [1]; ;
  1. Gulf Mineral Resources Co., Albuquerque, NM
Scanning-electron-microscope study of authigenic minerals in the Westwater Canyon Member of the Morrison Formation (Upper Jurassic) indicates that compositional variations exist within and adjacent to sandstone-type uranium deposits. Montmorillonite is the dominant clay mineral downdip of the orebody; chlorite is enriched in the ore zones, and kaolinite and altered montmorillonite are enriched in ground updip of the ore. The data also suggest that clay minerals, not pyrite or hematite, may locally be the iron-bearing species of importance. While it is not possible to positively identify organic materials in SEM (scanning-electron microscope) photomicrographs, materials deduced to be organic in nature postdate the beginning of authigenic clay formation. This implies that these materials may be carriers of uranium in the ground-water system from which the ore deposits precipitated. Identification of patterns of clay-mineral alteration and the role that organic materials might play as transporting media could significantly alter exploration techniques. These patterns may be especially useful tools in areas where the orebodies are known to be removed from the iron-species redox interface.
OSTI ID:
6135230
Report Number(s):
CONF-7905120-
Conference Information:
Journal Name: Mem. - N.M. Bur. Mines Miner. Resour.; (United States) Journal Volume: 38
Country of Publication:
United States
Language:
English