青海东昆仑清水河地区多金属矿成矿规律及找矿远景分析

Metallogenic regularity and prospecting prospect of polymetallic ore deposits in Qingshui River area, East Kunlun, Qinghai

青海东昆仑清水河地区的成矿受断裂的影响显著,并且在该地区发现了很多金属矿。在岩浆活动中,由于受到断裂构造以及花岗闪长岩的侵入,会有气水溶液从岩浆中分离出来,沿着万保沟中基性火山岩的构造进行活动,通过沉淀等成矿作用,在清水河地区形成了多金属矿点。本文通过对清水河矿区地质特征及成矿条件进行分析,探讨了该区成矿规律及找矿远景。

The mineralization of the Qingshui River area in East Kunlun, Qinghai province is obviously affected by faults, and many metallic minerals have been found in this area. In magmatic activities, as a result of the intrusion of faults and granodiorite, will be separated from the gas water solution from the magma, 000 tectonic activities along the volcano rock foundation ditch, the precipitation of mineralization in the Qingshui River area, the formation of multi metal ore. Based on the analysis of geological characteristics and metallogenic conditions of Qingshui River mining area, the metallogenic regularity and prospecting prospect of this area are discussed.