新疆琼库都克铜多金属矿地质特征与找矿标志

Geological Characteristics and Prospecting Signs of Qiongkuduke Copper Polymetallic Deposit,Xinjiang

矿区成矿物质主要来源是下石炭统雅满苏组火山碎屑岩地层。构造发育为矿质元素的富集提供了容矿场所,岩体与地层的接触部位或岩体本身内部往往形成较为有利的矿化富集地段。地质、围岩蚀变等找矿标志明显,研究结果为以后的地质勘查提供一定的参考。

The main source of ore-forming materials in the mining area is the volcanic clastic stratum of the Lower Carboniferous Yamansu Formation.Tectonic development provides an ore-holding place for the enrichment of mineral elements.The contact part between the rock mass and the stratum or the interior of the rock mass itself often forms a more favorable mineralized enrichment section.Geological and surrounding rock alteration signs are obvious,and the research results provide a certain reference for future geological surveys.