新疆萨热克铜矿成矿地质特征及找矿探讨

Discussion on geological characteristics and ore prospecting Sareke copper deposit in Xinjiang

萨热克铜矿位于塔里木盆地西南中新生代蚴陷西北缘的次级盐地-托云盆地的两缘,矿体分布在下白垩统第三岩性段,矿床主要受控于N E向向斜构造与层间断裂。矿体呈层状赋存于白垩系特定的层位和碎屑岩建造中,属于沉积-改造型砂砾岩铜矿。萨热克铜矿铜矿是新疆地区一种非常重要的矿床类型。通过对该铜矿成矿地质特征及找矿潜力进行分析,认为本区具有良好的找矿前景。

The secondary salt Sareke copper deposit is located in the southwestern Tarim Basin in Cenozoic basin in the northwestern margin of the Tuyon basin margin - two, the distribution of ore bodies in the lower Cretaceous third lithologic deposits, mainly controlled by N E to the syncline structure and interlayer fracture. The ore bodies are bedded in the specific stratum and clastic rock formation of the Cretaceous, which belongs to the sedimentary transformation of the sand and gravel copper deposits. The Sareke copper deposit is an important deposit types in Xinjiang area. Based on the analysis of the geological characteristics and prospecting potential of the copper deposit, it is considered that this area has good prospecting potential.