喀什地区主要铅锌矿床地质特征及成因探讨  

The Geological Characteristic And Origin of Major Lead-Zinc Ore Deposits in Kas-gar region

作　　者：彭守晋 

机构地区：[1]新疆有色地质研究所

出　　处：《新疆有色金属》1990年第2期8-16,共9页

摘　　要：南疆喀什地区是新疆寻找铅锌矿的一个重要远景区,巳知主要矿床均分布于南天山冒地槽褶皱带西段,塔里木地台西北和西南缘。本文首次对该区铅锌矿床成因进行了探讨并提出了今后找矿方向。Kas-gar region of southern Xinjiang is one of the important potential promising areas in Xinjiang for, searching Lead-Zinc doposits, The major ore deposits are fundamentaly distributed in the western part of Southern Tianshan miogeosynclinal fold belt, North-west and South-west margin of Tarimplatform. In this paper first have discussed the genesis of ore deposit and also pointed out the main direction of future ore-searching in the region.

关 键 词：铅锌矿床 地质特征 塔里木地台 矿床成因类型 锌矿 白云岩化 冒地槽 布拉克 里塔 卡兰 

分 类 号：TG146[一般工业技术—材料科学与工程]