Possible uranium mineralization, Mineral Mountains, Utah

Open-File Report 79-1354
By: , and 



The Mineral Mountains block in west-central Utah is a horst whose core stands structurally high relative to all nearby basin-and-range fault blocks. Rocks of the Mineral Mountains range from Precambrian to Quaternary in age, but mostly consist of Tertiary granitic rocks. The range lies with the Wah Wah-Tusher mineral belt. Lead, silver, gold, and tungsten have been mined commercially. During a geochemical survey conducted in the summer of 1978, 30 water samples and 29 stream-sediment samples were collected from the Mineral Mountains area. The interpretation of simple plots of uranium concentrations and the results of a Q-mode factor analysis indicate that potential exists for uranium mineral deposits within the Mineral Mountains. The most favorable areas are in the granitic pluton near its contacts with sedimentary and metamorphic rocks. The most likely source of the uranium anomalies is uraninite-bearing epigenic veins along faults and fractures within the pluton. Three hypothetical models are proposed to account for the uranium mineralization.

Additional publication details

Publication type Report
Publication Subtype USGS Numbered Series
Title Possible uranium mineralization, Mineral Mountains, Utah
Series title Open-File Report
Series number 79-1354
DOI 10.3133/ofr791354
Edition -
Year Published 1979
Language ENGLISH
Publisher U.S. Geological Survey,
Description iii, 48 p. :ill., maps ;29 cm.
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