青海省夏日哈—什多龙地区地质特征及铜多金属矿床成矿特点浅析

The geological characteristics and metallogenic characteristics of the copper polymetallic deposit in summer in Qinghai province

该地区大地构造位置处于秦祁昆造山系(IV)柴北缘结合带(IV-5)和东昆仑弧盆系(IV-8)。文章通过对该地区地质特征及典型矿床分析总结了该地区主要矿床成因特点,希望能对该地区寻找矿床资源提供帮助。

The tectonic location of the region is located in the zone （IV-5） and the eastern kunlun arc basin （IV-8） in the qinqi-kun orogenic system （IV）.Through the analysis of geological features and typical deposits in this area, the genetic of the main deposits in the region, and hopes to provide some help for the exploration of mineral deposits in the region.