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National Uranium Resource Evaluation, Ogden Quadrangle, Utah and Wyoming

Michael E. Madson, W R Reinhart

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Abstract

The Ogden 1/sup 0/ x 2/sup 0/ Quadrangle was evaluated using National Uranium Resource Evaluation criteria to determine environments favorable for the occurrence of uranium deposits. Geologic reconnaissance, geochemical sampling, airborne radiometric and hydrogeochemical data interpretation, detailed surface studies, and subsurface investigations were conducted. The Crawford Mountains, northern Fossil Basin and Darby Thrust zone areas were delineated as favorable. Within these areas, the Meade Peak Phosphatic Shale Member of the Permean Phosphoria Formation contains an environment favorable for Phosphoria-type uranium deposits. All other environments in the quadrangle are unfavorable for uranium deposits. The Bannock and Absaroka Thrust zones are unevaluated because of inadequate subsurface geologic information.

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What this paper is about

The Ogden 1/sup 0/ x 2/sup 0/ Quadrangle was evaluated using National Uranium Resource Evaluation criteria to determine environments favorable for the occurrence of uranium deposits. Geologic reconnaissance, geochemical sampling, airborne radiometric and hydrogeochemical data interpretation, detailed surface studies, and subsurface investigations were conducted. The Crawford Mountains, northern Fossil Basin and Darby Thrust zone areas were delineated as favorable. Within these areas, the Meade Peak Phosphatic Shale Member of the Permean Phosphoria Formation contains an environment favorable for Phosphoria-type uranium deposits. All other environments in the quadrangle are unfavorable for uranium deposits. The Bannock and Absaroka Thrust zones are unevaluated because of inadequate subsurface geologic information.

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Available abstract

The Ogden 1/sup 0/ x 2/sup 0/ Quadrangle was evaluated using National Uranium Resource Evaluation criteria to determine environments favorable for the occurrence of uranium deposits. Geologic reconnaissance, geochemical sampling, airborne radiometric and hydrogeochemical data interpretation, detailed surface studies, and subsurface investigations were conducted. The Crawford Mountains, northern Fossil Basin and Darby Thrust zone areas were delineated as favorable. Within these areas, the Meade Peak Phosphatic Shale Member of the Permean Phosphoria Formation contains an environment favorable for Phosphoria-type uranium deposits. All other environments in the quadrangle are unfavorable for uranium deposits. The Bannock and Absaroka Thrust zones are unevaluated because of inadequate subsurface geologic information.

Key concepts: Quadrangle, Geology, Uranium, Isopach map, Radiometric dating, Geochemistry, Mining engineering, Uranium ore

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