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锑矿化集中于喜马拉雅期石英斑岩内接触带,存在矿源层形成、充分分异及近地表成矿三个阶段。可作为滇西碱性岩锡矿床典型。
Antimony mineralization concentrates on the contact zone of the quartzite porphyry in the Himalayan period, which is characterized by the formation of mineralized layers, well-differentiated and near-surface mineralization. It can be used as a typical alkali-rock tin deposit in western Yunnan.