Reassessment of Equilibrium Temperatures of Rehai (Hot Sea) Geothermal Field, Tengchong County, Yunnan Province, China
- Location
- Rehai, China
- Conference
- New Zealand Geothermal Workshop
- Year
- 1990
- Session
- Geochemistry
- Language
- English
Full text
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Abstract
The reservoir temperature of Rehai geothermal field has been est imated from various mometers. The average temperature i n the shal reservoir , which occurs in a weathered yer at t h e top of a Late Cretaceous granite , is about deeper i n t h e t h i s g r a n i t e , it i s about The temperature of parent water in the deep reservoir is about
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