Determination of timing of recharge for geothermal fluids in the Great Basin using environmental isotopes and paleoclimate indicators
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Authors
Buchanan, Paul K.
Issue Date
1990
Type
Thesis
Language
en_US
Keywords
Hydrology , Water , Geothermal , Recharge , Precipitation , Paleorecharge , Isotopic Studies , Great Basin , Thermal Water , Range Bounding Faults , Isotope Fractionation , Unstable Light Isotopes , Pleistocene , Ground-water , Mackay Theses and Dissertations Grant Collection
Alternative Title
Abstract
Research indicates that the fluid source for geothermal system recharge in the Great Basin is paleorecharge.
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.
Citation
Publisher
University of Nevada, Reno
License
In Copyright(All Rights Reserved)