Fluid-mineral equilibria in a hydrothermal system, Roosevelt hot springs, Utah

Author:

Capuano Regina M.,Cole David R.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference53 articles.

1. Aquifer chemistry of four high-temperature geothermal systems in Iceland;Arnorsson;Geochim. Cosmochim. Acta,1978

2. Hydrothermal alteration at the Roosevelt Hot Springs thermal area, Utah: Characterization of rock types and alteration in Getty Oil Company Well Utah State 52-21;Ballantyne;Univ. of Utah Dept. of Geology and Geophysics Topical Rep. No. 78-1701.a. 1.1.4, DOE/DGE contract No. EG-78-C-07-1701,1978

3. Hydrothermal alteration at the Roosevelt Hot Springs thermal area, Utah: modal mineralogy, and geochemistry of sericite, chlorite, and feldspar from altered rocks, Thermal Power Company well Utah State 14-2;Ballantyne;Univ. of Utah Dept. of Geology andGeophysics Rep. No. 78-1701.a.1.15, DOE/DGE contract No. EG-78-C-07-1701,1978

4. Geochemistry of sericite and chlorite in well 14-2 Roosevelt Hot Springs geothermal system and in mineralized hydrothermal systems;Ballantyne;Univ. of Utah Dept. Geology and Geophysics Rep. No. 79-1701.a.1.6, DOE/DGE contract No. DE-AC07-78ET/ 28392,1980

5. Hydrothermal alteration at the Roosevelt Hot Springs thermal area, Utah: Petrographic characterization of the alteration at 2 kilometers depth;Ballantyne;Univ. of Utah Dept. of Geology and Geophysics Tech. Rep. No. 78-1701.a.1.1, DOE/DGE contract No. EG-78-C-07-1701,1978

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