Structure of geothermal reservoirs and the temperature of mantle-derived magma hot source in the Rehai area, Tengchong

Acta Petrologica Sinica

Volumn 16, Issue 1, 2000, Pages 83-90

  Shangguan, Z ^a  

^a INSTITUTE OF GEOLOGY   (China)

Author keywords

Geothermal fluid; Geothermometer; Isotope; Magma hot source

Indexed keywords

CARBON DIOXIDE; GEOTHERMAL FIELDS; MERCURY (METAL);

GEOTHERMAL FLUIDS; GEOTHERMAL RESERVOIR; GEOTHERMOMETERS; ISOTOPIC FRACTIONATIONS; MAGMA HOT SOURCE; MANTLE DERIVED MAGMAS; MULTI-LAYERED STRUCTURE; SHALLOW RESERVOIRS;

ISOTOPES;

GEOTHERMAL ENERGY; GEOTHERMAL SYSTEM; GEOTHERMOMETRY; HEAT SOURCE; MANTLE;

CHINA;

EID: 84977975212     PISSN: 10000569     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (11)

1. The inference of magmatic heat source beneath the Rehai field of Tengchong from the result of magnetotelluric sounding
2. The isotope geochemistry of water and carbon in geothermal areas
3. Geochemistry in geothermal exploration
4. Stable carbon isotope ratio and the existence of a gas phase in the evolution of carbonate ground water
5. A revised equation for the Na/K geothermometer
6. Modern hot spring geochemistry at the Tanlu fault and Jiaoliao block in eastern China
7. 2 content dissolved in geothermal fluid
8. The genetic classification of modern geothermal fluid activity at the Tengchong area in Yunnan
9. Material sources of escaped gases from Tianchi volcanic geothermal area, Changbai Mountains