Hydrothermal alteration in two deep exploratory wells in Dixie Valley, Nevada

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Author
Bard, Thomas R.
Advisor
Slemmons, D.B.
Date
1980
Type
Thesis
Department
Geological Sciences and Engineering
Degree Level
Master's Degree
Degree Name
Geology
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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/11714/1104
Subject
geothermal
hydrothermal
alteration
fluids
clays
kaolinite
chlorite
illite
high-angle normal faults
normal faults
structures
wells
boreholes
Mackay Science Project
 
Additional Information
Committee MemberLarson, L. T.
RightsIn Copyright
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