The stratiform skarns of hydrothermal fluid sedimentary origin are well developed in Kendekoke gold deposit, Qinhai province.
热水沉积成因层矽卡岩在青海省肯德可克金矿区非常发育。
The stratiform skarns of hydrothermal fluid sedimentary origin are well developed in Kendekoke gold deposit, Qinhai province.
热水沉积成因层矽卡岩在青海省肯德可克金矿区非常发育。
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