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Calc-silicate mineralization in active geothermal systems

Technical Report ·
DOI:https://doi.org/10.2172/5794604· OSTI ID:5794604
The detailed study of calc-silicate mineral zones and coexisting phase relations in the Cerro Prieto geothermal system were used as examples for thermodynamic evaluation of phase relations among minerals of variable composition and to calculate the chemical characteristics of hydrothermal solutions compatible with the observed calc-silicate assemblages. In general there is a close correlation between calculated and observed fluid compositions. Calculated fugacities of O{sub 2} at about 320{degrees}C in the Cerro Prieto geothermal system are about five orders of magnitude less than that at the nearby Salton Sea geothermal system. This observation is consistent with the occurrence of Fe{sup 3+} rich epidotes in the latter system and the presence of prehnite at Cerro Prieto.
Research Organization:
Stanford Univ., CA (USA). Dept. of Geology; California Univ., Riverside (USA). Inst. of Geophysics and Planetary Physics; Michigan Technological Univ., Houghton (USA). Dept. of Geology and Geological Engineering
DOE Contract Number:
FC07-80ID12145
OSTI ID:
5794604
Report Number(s):
UCR/IGPP-83/7; ON: DE83016724
Country of Publication:
United States
Language:
English