摘要
预查区位于柴达木盆地南缘,地处东昆仑南造山带东段。区内出露主要为中—新元古代万保沟群及晚古生代石炭系哈拉郭勒组地层。区内构造控矿特征明显,断裂构造与成矿关系密切,属控矿构造。
The pre-inspection area is located in the southern margin of the Qaidam Basin and the eastern segment of the southern East Kunlun orogenic belt.The main outcrops in the area are the Meso-Neoproterozoic Wanbaogou Group and the Late Paleozoic Carboniferous Halaguole Formation.The tectonic ore-controlling characteristics are obvious in the area,and the fault tectonics are closely related to mineralization.
作者
王珩
王靖
WANG Heng;WANG Jing(Qinghai nonferrous metals Third Geological Exploration Institute,Xining 810000,China)
出处
《世界有色金属》
2021年第5期95-96,共2页
World Nonferrous Metals
关键词
铅多金属矿床
地质特征
成矿远景
充填热液型
lead polymetallic deposit
geological characteristics
metallogenic prospect
filling hydrothermal type
