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Hydrothermal alteration in two deep exploratory wells in Dixie Valley, Nevada
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Mackay028_Bard.pdf
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Date
1980Type
ThesisDepartment
Geological Sciences and Engineering
Degree Level
Master's Degree
Degree Name
Geology
Abstract
Local concentrations of kaolinite characterize fissures, which are actively conducting hydrothermal fluids in Dixie Valley.
Description
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.
Permanent link
http://hdl.handle.net/11714/1104Additional Information
Committee Member | Larson, L. T. |
---|---|
Rights | In Copyright |
Rights Holder | Author(s) |