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Infiltration uranium deposits in ash flow tuffs
Date
1972Type
ThesisDepartment
Geological Sciences and Engineering
Degree Level
Master's Degree
Degree Name
Geology
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
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Permanent link
http://hdl.handle.net/11714/1375Additional Information
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