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April 01, 1993
Paleogeothermal and paleohydrologic conditions in silicic tuff from Yucca Mountain, Nevada Available to Purchase
David L. Bish;
David L. Bish
Los Alamos National Laboratory, Earth and Environmental Sciences Division, Los Alamos, NM, United States
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James L. Aronson
James L. Aronson
Case Western Reserve University, United States
Search for other works by this author on:
David L. Bish
Los Alamos National Laboratory, Earth and Environmental Sciences Division, Los Alamos, NM, United States
James L. Aronson
Case Western Reserve University, United States
Publisher: Clay Mineral Society
First Online:
02 Mar 2017
Online ISSN: 1552-8367
Print ISSN: 0009-8604
GeoRef, Copyright 2004, American Geological Institute.
Clays and Clay Minerals (1993) 41 (2): 148–161.
Article history
First Online:
02 Mar 2017
Citation
David L. Bish, James L. Aronson; Paleogeothermal and paleohydrologic conditions in silicic tuff from Yucca Mountain, Nevada. Clays and Clay Minerals 1993;; 41 (2): 148–161. doi:
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Index Terms/Descriptors
- clay mineralogy
- clay minerals
- fluid inclusions
- geologic thermometry
- high-level waste
- hydrothermal alteration
- hydrothermal conditions
- igneous rocks
- illite
- inclusions
- metasomatism
- Nevada
- Nye County Nevada
- pyroclastics
- radioactive waste
- sheet silicates
- silicates
- siliceous composition
- smectite
- tuff
- United States
- volcanic rocks
- waste disposal
- Yucca Mountain
Latitude & Longitude
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