内蒙古上关家沟铜银多金属矿矿体地质特征及找矿标志

Geological characteristics and prospecting signs of copper and silver polymetallic ore deposits in Inner Mongolia

研究区位于大兴安岭隆起带与松辽坳陷盆地的过渡带上和滨西太平洋陆缘活化带的交汇部位,为矿产形成提供了有利空间。本文在对研究区地质概况进行分析基础上,进而对矿化蚀变带特征,矿石质量及矿石类型,围岩蚀变及矿化特征进行深入分析,最后对矿床成因类型及找矿标志进行研究,对研究区以后的地质勘查工作具有很重要指导意义。

The research area is located at the intersection of the transition belt of the daxinganling uplift belt and the songliao depression basin and the zone of the activation belt of the continental margin of the Pacific Ocean, which provides a favorable space for mineral formation. the geological survey in the study area, and the mineralized alteration zone characteristics, mineralization features in-depth analysis, the study of genetic types of ore deposit, and prospecting marks, and later of geological exploration in the studied area has very important significance.