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昆仑气铅锌矿床位于伊春-延寿铁多金属成矿带北段,矿体赋存于燕山晚期闪长玢岩与寒武系下统铅山组大理岩接触带及其内外带的矽卡岩中。矿床成因类型为岩浆期后矽卡岩型。矽卡岩、圈岩蚀变、物化探异常为重要的找矿标志。
The Kunlun gas lead-zinc deposit is located in the northern section of the Yichun-Yanzuo iron-polymetallic metallogenic belt. The ore body occurs in the marble contact zone of the Yanshanian marble and the skulls Rock. The genetic type of the deposit is skarn type after magmatic period. Skarn, ring rock alteration, physical and geochemical anomalies as an important indicator of prospecting.