库地铬铁矿地质特征及西昆仑北蛇绿岩带铬铁矿成矿远景探讨  

The Geological Characteristics、Tectonic Setting of Kudi Chromite and Ore-prospect in Northern Edge of Western KunLun

作　　者：李军[1] 陈强[1] 赵献军[1] 刘洋旭[1] 张伟[1] 王波[1] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第六地质大队,新疆哈密839000

出　　处：《新疆地质》2012年第3期304-306,共3页Xinjiang Geology

摘　　要：西昆仑地区是国内最重要的超基性岩出露区之一,原生的铬铁矿均与超基性岩有关。库地蛇绿岩中发现了具工业意义的铬铁矿体,以库地蛇绿岩铬铁矿为典型矿床,对整条西昆仑北蛇绿岩带进行成矿远景探讨,以期对该区域铬铁矿找矿工作起指导作用。The western KunLun is one of the most important areas where the ultramafic rocks is distributed,the native chromitite is related to the ultramafic rocks.Ophiolitic chromitite prospecting in the northern edge of the western KunLun which is on the basis of Kudi ophiolitic chromitite will be a valuable direction for chromite exploration.

关 键 词：西昆仑 蛇绿岩带 铬铁矿 地质特征 成矿远景 

分 类 号：P618.31[天文地球—矿床学] P618.33[天文地球—地质学]