Based on geological environment, bi-model volcanic series, sedimentary formation and geochemical features of volcanic rocks, it is held that the deposits were most probably formed in the Carboniferous back arc rifted environment.

 
  • 根據礦床產(chǎn)出地質(zhì)環(huán)境、雙峰式火山巖系、沈積建造以及火山巖地球化學(xué)特征,推斷昆侖式火山巖型塊狀硫化物銅礦床最可能形成于泥盆紀-石炭紀弧后拉張構造環(huán)境。
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