Variation in sericite compositions from fracture zones within the Coso Hot Springs geothermal system
Open Access
- 1 May 1987
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 51 (5) , 1245-1256
- https://doi.org/10.1016/0016-7037(87)90216-x
Abstract
No abstract availableThis publication has 27 references indexed in Scilit:
- A chlorite solid solution geothermometer the Los Azufres (Mexico) geothermal systemContributions to Mineralogy and Petrology, 1985
- Calc-silicate mineralization in active geothermal systemsEconomic Geology, 1984
- Activity/Composition Relations among Silicates and Aqueous Solutions: II. Chemical and Thermodynamic Consequences of Ideal Mixing of Atoms on Homological Sites in Montmorillonites, Illites, and Mixed-Layer ClaysClays and Clay Minerals, 1983
- Fluid-mineral equilibria in a hydrothermal system, Roosevelt hot springs, UtahGeochimica et Cosmochimica Acta, 1982
- Theoretical prediction of phase relations among aqueous solutions and minerals: Salton Sea geothermal systemGeochimica et Cosmochimica Acta, 1981
- Heat flow in the Coso Geothermal Area, Inyo County, CaliforniaJournal of Geophysical Research, 1980
- Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, CaliforniaJournal of Geophysical Research, 1980
- Hydrothermal Alteration in Active Geothermal FieldsAnnual Review of Earth and Planetary Sciences, 1978
- The Ohaki-Broadlands hydrothermal area, New Zealand; mineralogy and related geochemistryAmerican Journal of Science, 1970
- Empirical Correction Factors for the Electron Microanalysis of Silicates and OxidesThe Journal of Geology, 1968