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Fluid geochemical constraints on the heat source and reservoir temperature of the Banglazhang hydrothermal system, Yunnan-Tibet Geothermal Province, China
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文摘
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.

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