Fluid geochemical constraints on the heat source and reservoir temperature of the Banglazhang hydrothermal system, Yunnan-Tibet Geothermal Province, China
作者单位：State Key Laboratory of Biogeology and Environmental Geology, Laboratory of Basin Hydrology and Wetland Eco-restoration & School of Environmental Studies, China University of Geosciences, 430074 Wuhan, Hubei, PR China
There is a lack of neutral chloride springs at Banglazhang. Banglazhang is likely to be above the margin of a magma chamber. The Banglazhang geothermal waters are not affected by the input of a magmatic fluid. This study is suggestive for identifying the geneses of unexplored hydrothermal systems.