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

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Authors

Bard, Thomas R.

Issue Date

1980

Type

Thesis

Language

en_US

Keywords

geothermal , hydrothermal , alteration , fluids , clays , kaolinite , chlorite , illite , high-angle normal faults , normal faults , structures , wells , boreholes , Mackay Science Project

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Abstract

Local concentrations of kaolinite characterize fissures, which are actively conducting hydrothermal fluids in Dixie Valley.

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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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