摘要
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。
The Wunugetu mountain copper deposit is located at northwest of deerbugan ore belt. Copper, molybdenum, lead and zinc constitute the main ore - forming elements. Further prospecting orientation in the zone was proposed based on the summary of geological character and characteristics and ore controlling regularities of the deposit.
出处
《长春工程学院学报（自然科学版）》
2009年第1期92-96,共5页
Journal of Changchun Institute of Technology：Natural Sciences Edition
关键词
外围找矿
前景探讨
内蒙古
乌努格吐山
exploration
surrounding prospect
Inner Mongolia
Wunugetu mountain
