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Geological and isotopic constraints on the origin of the Anle carbonate-hosted Zn-Pb deposit in northwestern Yunnan Province, SW China
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文摘

Sulfur may have been derived from evaporites.

Carbon and metals may have been sourced from the ore-hosting dolostone that was affected by the Songpan–Ganzi orogenic event.

Zn isotopes can't be used as useful tracers for ore-forming metals and discriminators for metallogenic setting.

The Anle Zn–Pb deposit can be assigned to be an epigenetic MVT deposit.

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