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Genesis of the Zhaxikang epithermal Pb-Zn-Sb deposit in southern Tibet, China: Evidence for a magmatic link
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文摘

The Zhaxikang Pb-Zn-Sb deposit resembles typical IS epithermal deposits.

The Pb-Zn-Sb mineralization is closely related to Fe-Mn carbonation and silicification.

Ar-Ar age, FIs and H-O-C isotopes imply genetic link between magmatic fluids and mineralization.

High regional geothermal gradient facilitated long distance magmatic fluid transportation.

Long distance fluid transport formed wide alteration zone and distal Pb-Zn-Sb mineralization.

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