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.
出处
《新疆地质》
CAS
CSCD
北大核心
2012年第3期304-306,共3页
Xinjiang Geology
关键词
西昆仑
蛇绿岩带
铬铁矿
地质特征
成矿远景
Western KunLun
Ophiolitic zone
Chromite
Geological characteristics
Ore-prospect
