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Review of progress in understanding the fluid geochemistry of the Cerro Prieto Geothermal System

Conference ·
OSTI ID:7369514
Fluid geochemistry has played a major role in the authors 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 mechanims, and production-induced aquifer boiling and cold-water entry. The extensive geochemical data and interpretation 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.
Research Organization:
Geological Survey, Menlo Park, CA
OSTI ID:
7369514
Report Number(s):
CONF-8208109-Vol.2-3; ON: DE87003674
Country of Publication:
United States
Language:
English