探析阿尔金南缘断裂带东段地质特征及找矿方向  

The eastern section of the geological characteristics and prospecting direction of South Altyn fault zone

作　　者：刘海龙 

机构地区：[1]新疆地矿局第二区域地质调查大队,新疆昌吉831100

出　　处：《世界有色金属》2017年第2期95-96,共2页World Nonferrous Metals

摘　　要：阿尔金南缘断裂带自形成以来,历经多次活动,是划分塔里木地台与东昆仑褶皱系的超岩石圈深断裂,不仅控制了区内多种岩浆岩、变质岩的分布,同时其产生的次级断裂构造也给各种成矿热液提供了滞存空间。The southern margin of the Altun fault zone since the formation, through many activities, is the division of the Tarim platform and East Kunlun fold system of ultra deep lithospheric fracture, not only control the distribution of a variety of magmatite, metamorphic rocks, secondary faults at the same time they are also for all kinds of ore-forming fluid provides the stagnant space.

关 键 词：阿尔金南缘断裂 火山岩铜矿 

分 类 号：P542.3[天文地球—构造地质学]