Kendekeke Co-Bi-Au deposit is a important cabolt-polymetallic deposit in east Kunlun metallogenic belt. 钴矿广泛应用于工业生产的各个领域,我国每年需要进口。
Kendekeke Fe-Co multi-metal deposit in Qinghai is located in the southwest edge of Qaidam basin and middle parts of Qimantage rear arc rift zone. 青海东昆仑肯德可克铁钴多金属矿床位于柴达木盆地西南缘,祁漫塔格弧后裂陷带中部。
Skarnization siliceous rocks in the lower Ordovician Tieshidasi group is one of the dominant host rocks of Kendekeke cobalt-gold deposit. 上奥陶统铁石达斯群夕卡岩化硅质岩是东昆仑肯德可克钴金矿床的主要围岩之一,具有沉积结构构造。
APPLICATION OF GEOPHYSICAL EXPLORATION METHOD IN KENDEKEKE MINE 青海省肯德可克矿区地球物理勘查方法的应用
