Latitude: 31°22'20"N
Longitude: 84°3'11"E
A large bittern-salt lake in the Gangdise Mountains in the interior of the Tibetan Plateau. The lake consists of two sub-basins, a southern and a northern one, which are joined by a narrow channel. The lake has a total area of 243km2, a mean depth of 70cm, and a maximum depth of less than 2m. The salt content of the lake water is 360-410g/l. The basin originated through faulted structures. The underlying bedrock is Cretaceous-Eogene acidic igneous rocks, mudstones and sandstones. A large area of playa is being exposed around the lake, and mirabilite is currently being deposited in the lake.
References
- Wen Qi and Mianping Zheng (1995): Sedimentary characteristics of ZK91-2 core and climate-environment evolution of Zabuye lake, Tibet plateau. Journal of Lake Sciences 77(2).
- Yu, G., Harrison, S.P., and Xue, B. (2001): Lake status records from China: Data Base Documentation. MPI-BGC Technology Report No. 4, pp. 183-190.
- Yong-Sheng Zhang, Mian-Ping Zheng, Zhen Nie, and Ling-Zhong Bu (2005): 15°C-Isothermal Evaporation Experiment on Carbonate-type Brine from Zabuye Salt Lake, Tibet, Southwestern China. Sea-lake Salt and Chemical Industry [Yanye Yu Huagong] 34(4), 1-5.
- Wen Qi and Mianping Zheng (2007): Simulation with Pitzer model of lake brine evolution of Zabuye salt lake, Tibetan plateau. Acta Geologica Sinica 81(12), 1734-1741.
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11 entries listed. 11 valid minerals. 1 type locality (valid mineral).
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