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铜厂铜钼矿位于哀牢山-金沙江富碱侵入岩带的最南段,处于哀牢山逆冲深大断裂与藤条河断裂所夹持的金平微地块内,与铜厂铜钼矿矿化有关的岩体的岩性主要为斑状角闪正长岩,斑状角闪正长岩为灰—肉红色,块状构造,似斑状,斑状结构,主要由正长石(50～70%)、斜长石(20～30%)、石英(5
Copper copper molybdenum mine is located in the Ailaoshan - Jinsha River alkali-rich intrusive rock belt in the southern section, in the Ailao thrust deep fault and the rattan River fault held by the gold-ping micro-block, and copper copper plant The lithology associated with molybdenum mineralization is mainly hornblende argillaceous, and the hornblende argillite is greyish-flesh-colored, block-like, patchy and porphyritic, mainly composed of orthoclase (50 ~ 70%), plagioclase (20 ~ 30%), quartz (5