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Geochemical features of the geothermal fluids from the Mapamyum non-volcanic geothermal system (Western Tibet, China)
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文摘

Detailed geochemical properties were investigated for the Mapamyum geothermal system, western Tibet.

The equilibrated reservoir temperature and the source of the solutes were analysed.

Strong mixing between cold meteoric water and deeply-seated thermal fluids occurred.

The carrier CO2 in hydrothermal water is mainly of a magmatic or metamorphic CO2 origin.

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