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Mineralogy and geochemistry of Mariano Lake uranium deposit, Smith Lake district

Conference · · Mem. - N.M. Bur. Mines Miner. Resour.; (United States)
OSTI ID:6033884
The Mariano Lake uranium deposit is located on the west side of the Smith Lake district in the Grants mineral belt. Mineralization is restricted to a basal arkosic sandstone of the Brushy Basin Member of the Morrison Formation (Upper Jrassic). This sandstone is equivalent to the Poison Canyon sandstone of the Ambrosia Lake district and contains a series of paleochannels that have been mineralized. The ore displays a roll-type geometry and is located at an iron-sulfur redox interface. The deposit is chemically different from other deposits of the grants mineral belt. It is characterized by low total carbon dioxide, calcium, molybdenum, and selenium, whereas sulfur and vanadium are enriched. Arsenic and zinc exhibit regular zoning patterns across the deposit. The deposit contains an ubiquitous assemblage of pyrite, kaolinite, chlorite, illite, and illite-montmorillonite associated with vanadiferous ore mixed with organic carbon. No primary uranium minerals have been identified. Gypsum (variety selenite) is present, but calcite is absent. The age of mineralization is unknown. The ore has been remobilized, perhaps more than once, and mineralization may have occurred during mid-Cretaceous, Laramide, or post-Laramide time. Based on existing data, polygenetic models are as reasonable as a single stage of remobilization.
OSTI ID:
6033884
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

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