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.
出处
《世界有色金属》
2017年第2期95-96,共2页
World Nonferrous Metals
关键词
阿尔金南缘断裂
火山岩铜矿
South Altyn fault
volcano rock copper mine