REVIEW OF PROGRESS IN UNDERSTANDING THE FLUID GEOCHEMISTRY OF THE CERRO PRIETO GEOTHERMAL SYSTEM.
January 1, 1982
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 geochemical data and interpretations published from 1964 to 1981 are reviewed and discussed.
Citation Information
| Publication Year | 1982 |
|---|---|
| Title | REVIEW OF PROGRESS IN UNDERSTANDING THE FLUID GEOCHEMISTRY OF THE CERRO PRIETO GEOTHERMAL SYSTEM. |
| 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 | 70011434 |
| Record Source | USGS Publications Warehouse |