Geochemistry of sericite and chlorite in well 14-2 Roosevelt Hot Springs geothermal system and in mineralized hydrothermal systems
Chemical compositions of chlorite and sericite from one production well in the Roosevelt geothermal system have been determined by electron probe methods and compared with compositions of chlorite and sericite from porphyry copper deposits. Modern system sericite and chlorite occur over a depth interval of 2 km and a temperature interval of 250/sup 0/C.
- Research Organization:
- Utah Univ., Salt Lake City (USA). Dept. of Geology and Geophysics
- DOE Contract Number:
- AC07-78ET28392
- OSTI ID:
- 5285752
- Report Number(s):
- DOE/ET/28392-43
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
15 GEOTHERMAL ENERGY
ABUNDANCE
CHEMICAL ANALYSIS
CHEMICAL COMPOSITION
CHEMISTRY
CHLORITE MINERALS
COPPER ORES
ELECTRON MICROPROBE ANALYSIS
FLUIDS
GEOCHEMISTRY
GEOTHERMAL FLUIDS
GEOTHERMAL WELLS
Geothermal Legacy
KGRA
MICA
MICROANALYSIS
MINERALOGY
MINERALS
NORTH AMERICA
ORES
ROCKS
ROCKY MOUNTAIN REGION
ROOSEVELT HOT SPRINGS
THERMAL WATERS
USA
UTAH
WELLS
ABUNDANCE
CHEMICAL ANALYSIS
CHEMICAL COMPOSITION
CHEMISTRY
CHLORITE MINERALS
COPPER ORES
ELECTRON MICROPROBE ANALYSIS
FLUIDS
GEOCHEMISTRY
GEOTHERMAL FLUIDS
GEOTHERMAL WELLS
Geothermal Legacy
KGRA
MICA
MICROANALYSIS
MINERALOGY
MINERALS
NORTH AMERICA
ORES
ROCKS
ROCKY MOUNTAIN REGION
ROOSEVELT HOT SPRINGS
THERMAL WATERS
USA
UTAH
WELLS