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1 Introduction Multi-metal contained Lead-zinc deposits in northeast Yunnan,China,is located in a joint place of the Circum-Pacific tectonic domain and Tethyan tectonic domain.This joint place is featured by complex geological structure,unique geological characteristic,and multiple lead-zinc mineral deposits,which are discretely and linearly distributed along the cracks of several main fracture zones.Most of the lead-zinc ores were filled into the surrounding
1 Introduction Multi-metal contained Lead-zinc deposits in northeast Yunnan, China, located in a joint place of the Circum-Pacific tectonic domain and Tethyan tectonic domain. This joint place is featured by complex geological structure, unique geological characteristic, and multiple lead-zinc mineral deposits, which are discretely and linearly distributed along the cracks of several main fracture zones. Host of the lead-zinc ores were filled into the surrounding