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礦石的礦物組成比較簡單，銅的硫化物主要為黃銅礦，其次為斑銅礦和輝銅礦，銅的氧化物主要為孔雀石，其次為藍(lán)銅礦為鈷，非金屬礦物為石英長石等.其次為綠泥石。黑母石 白云母角閃石 方解石 方柱石。硫化礦物中黃鐵礦多呈細(xì)脈浸染及散點(diǎn)狀產(chǎn)出，次為囊狀重填，嵌布粒度為0.3~0.01 小于0.016毫米者占16%~30% 氧化物中的孔雀石大多呈薄膜狀沿解離和裂隙產(chǎn)出，伴生金屬礦物呈散點(diǎn)狀或細(xì)脈狀產(chǎn)出，在晶洞內(nèi)或較大裂隙面上孔雀石有時結(jié)晶成針狀放射狀集合體，礦物嵌布粒度為0.4~0.016毫米！ 

\The mineral composition of the ore is relatively simple, mainly for copper sulfide chalcopyrite, bornite and followed by chalcocite, copper oxide is mainly malachite, azurite followed by cobalt, non-metallic mineral quartz long stone, etc. followed by chlorite. Female black female Shi Baiyun hornblende calcite square pillar. Mostly sulfide minerals pyrite veinlets and disseminated scattered punctate output, time for cystic refill, dissemination size of less than 0.3 to 0.01 0.016 mm accounted for 16% to 30% was mostly oxides malachite film-like dissociation and fissures along outputs associated metals minerals were scattered spots or thin veins output, or large cracks in the surface of the crystal cave malachite sometimes radial needle crystal aggregates, minerals disseminated particle size 0.4 to 0.016 mm!

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