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位于得尔布干成矿带西北侧的乌努格吐山大型斑岩铜矿北东侧15km南山铜矿点,土壤异常以Cu、Mo、As为主,伴生Ag、Pb、Zn。异常带状面型分布,浓集中心明显,具水平分带,是一套反映斑岩型铜钼矿床前缘晕的组合异常;经中锑充电率等方法验证获得异常与化探异常吻合极好,定性为矿异常;通过钻孔验证发现铜钼矿体。推测矿床成因为斑岩型铜钼矿床,找矿前景乐观。
Pb, Zn is mainly associated with Cu, Mo and As in the Nanshan copper deposit located 15 km to the north east of the Uluguguoshan large porphyry copper deposit on the northwestern side of the Deerbugan metallogenic belt. The distribution of anomalous zonal surfaces with obvious concentration centers and horizontal zonation is a set of combination anomalies that reflect the front halo of the porphyry copper-molybdenum deposit. The abnormal anomalies coincide with geochemical anomalies Well, characterized as a mine anomaly; copper-molybdenum ore bodies were found by drilling validation. It is speculated that the genesis of the deposit is a porphyry copper-molybdenum deposit and the prospect of prospecting is optimistic.