Overview of calcite/opal deposits at or near the proposed high-level nuclear waste site, Yucca Mountain, Nevada, USA: Pedogenic, hypogene, or both?

Author:

Hill C. A.,Dublyansky Y. V.,Harmon R. S.,Schluter C. M.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous),General Engineering,General Environmental Science,Water Science and Technology,Environmental Chemistry

Reference65 articles.

1. Archambeau CB and Price MT (1991) An assessment of J. S. Szymanski's conceptual hydro-tectonic model and its relevance to hydrologic and geologic processes at the proposed Yucca Mountain nuclear waste repository. US Department of Energy, Minority Report, Special DOE Review Panel, unpaged

2. Bachman GO and Machette MN (1977) Calcic soils and calcretes in the southwestern United States. US Geol. Survey Open File Report 77-794. 163 pp

3. Bish DL (1989) Evaluation of past and future alterations in tuff at Yucca Mountain, Nevada, based on the clay mineralogy of drill cores USWG-1, G-2, and G-3. Los Alamos National Laboratory LA-10667-NS. 40 pp

4. Bish DL and Aronson JL (1993) Paleogeothermal and paleohydrologic conditions in silicic tuff from Yucca Mountain, Nevada. Clays Clay Minerals 41(2): 148–161

5. Brogan GE, Kellogg, KS, Slemmons DB, and Terhune CL (1991) Late Quaternary faulting along the Death Valley-Furnace Creek fault system, California and Nevada. US Geological Survey Bulletin 1991. 23 pp

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