关于塔卡提铅锌矿地质特征与成因分析

Geological characteristics and genetic analysis of Taka Ti Pb Zn deposit

西昆仑塔木-卡兰古铅锌铜成矿构造带是该矿的大地构造位置所在,属于西昆仑褶皱带克孜勒陶-库尔良铜铅锌多金属成矿带。区内的地层对矿床起着明显的控制作用,同时也受多种因素的影响。带去断裂构造主要呈现北东、西南向,控制着区内的矿体,卡拉巴西踏克组(石炭统)是矿体的主要赋存部位。砂岩以及白云质灰岩等与之关系密切,地层对其控制比较明显,矿体主要分布在蚀变特征突出及破碎明显的区域。文中分析了该矿的地质特征,对其矿床成因进行探讨,旨在对区内找矿工作有所帮助。

The Tarim Karan paleo lead zinc copper metallogenic belt in Western Kunlun is the location of the geodetic tectonic zone,and belongs to the kiz kurta-kurlian copper lead zinc metallogenic belt in the West Kunlun fold belt.The strata in the area play an important role in controlling the deposits,and are also affected by many factors.The fault zone is mainly located in the North East and southwest direction,and controls the orebodies in the area.The Cara Brazil formation(Carboniferous)is the main location of the ore body.Sandstone and dolomitic limestone are closely related to it,and strata control is more obvious.The ore bodies are mainly distributed in the areas where alteration features are prominent and broken obviously.The geological characteristics of the deposit are analyzed,and the genesis of the deposit is discussed in order to help the prospecting work in the area.