浅谈帕合堡铅锌矿矿床特征及成矿远景

A Brief Talk on the Characteristics and Metallogenic Prospect of the Pahebao Lead-Zinc Deposit

帕合堡铅锌矿矿床大地构造位置主要位于西昆仑中间地块及显生宙岩浆弧带上,工区北东与铁克里克陆缘隆起带交接。成矿区划属昆仑山腹地Au、Pb、Zn、Cu、Sn、Sb、As、Bi稀有、稀土金属、宝石成矿带的一部分。帕合堡铅锌矿矿床已圈出6个矿化蚀变带,矿脉规模较小,品位较高,是一个经济价值较高,适合硐采的小型铅锌多金属矿床。

The geotectonic location of the Pahebao lead-zinc deposit is mainly located in the middle block of the West Kunlun Mountains and the Phanerozoic magmatic arc belt,and the northeastern part of the work area is connected with the Tiekelike continental margin uplift belt.The metallogenic division is a part of Au,Pb,Zn,Cu,Sn,Sb,As,Bi rare,rare earth metals and gemstone metallogenic belt in the hinterland of Kunlun Mountains.The Pahebao lead-zinc deposit has been divided into six mineralization alteration zones.The vein is small in size and high in grade.It is a small lead-zinc polymetallic deposit with high economic value and is suitable for tunnel mining.