A review of progress in understanding the fluid geochemistry of the Cerro Prieto geothermal system
Fluid geochemistry has played a major role in our present understanding of the Cerro Prieto geothermal system. Fluid chemical and isotopic compositions have been used to indicate the origin of water, salts and gases, original subsurface temperature and fluid flow, fluid-production mechanisms, and production-induced aquifer boiling and cold-water entry. The extensive geochemical data and interpretations for Cerro Prieto published from 1964 to 1981 are reviewed and discussed. Fluid geochemistry must continue to play an important role in the further development of the Cerro Prieto field. ?? 1984.
Citation Information
Publication Year | 1984 |
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Title | A review of progress in understanding the fluid geochemistry of the Cerro Prieto geothermal system |
DOI | 10.1016/0375-6505(84)90007-5 |
Authors | A.H. Truesdell, N.L. Nehring, J. M. Thompson, C. J. Janik, T. B. Coplen |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Geothermics |
Index ID | 70013521 |
Record Source | USGS Publications Warehouse |