Active geothermal field, comprising 62 hot spring groups occurring along a NS-striking main fault. Country rocks in the area are mainly late Cretaceous granitoids, with minor late Tertiary and Quaternary volcanics, sandstone and conglomerate. The field is sub-divided in a northeast and a southwest section, referred to as the Huangguaqing-Liuhuangtang and Reshuitang fields, respectively.
Located around 10-15 km south of Tengchong.
References
- Qijia Zang (1984): On the origin of violarite from Halatonggou, Xinjiang and carrollite from Futuyu, Hebei, China. Acta Mineralogica Sinica 4(1), 74-77.
- Zhao, P., and Liao, Z. (1995): Preliminary gas and isotope geochemistry in the Rehai geothermal field, P.R. China. Proceedings of the 17th NZ Geothermal Workshop, 87-90.
- Pin'an Wang (2001): Geology and geochemistry of geothermal fields and hot-spring type gold deposits in Sanjiang orogen, southwestern China. Bulletin of the Geological Survey of Japan 52(8), 327-345 (in Japanese with English abstract).
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