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铜矿体赋存于石英二长斑岩中,普登群(PtlP)变粒岩为其围岩,矿化及岩性均可分带,其成因应属斑岩型铜矿叠加后期变质热液改造型多金属矿床,具有找到中大型金铜多金属矿床的潜力。
The copper ore body occurs in the quartz porphyritic. The PtlP granulite is characterized by its surrounding rock, mineralization and lithology. The genesis of the PtlP granulite should belong to the late metamorphic heat of the superimposition of porphyry copper deposits Liquid-modified polymetallic deposits, with the potential to find large gold-copper polymetallic deposits.