Infiltration uranium deposits in ash flow tuffs
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en_US
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Abstract
Four uranium deposits in the basal, carbonaceous zones of certain ash-flow tuffs of the Hartford Hill Rhyolite have been studied. Results indicate the uranium may have been leached, transported by groundwater, and concentrated in areas of organic debris. A conceptual model of the typical infiltration uranium deposit is presented and variations in the basic model are discussed.
Description
Thesis Number: 657.
Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.
Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.
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University of Nevada, Reno
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In Copyright(All Rights Reserved)