摘要
青海省都兰县和洛佳矿区主要寻找金多金属矿物,矿区位于东昆仑中段哈图沟地区,处于昆中昆南断裂之间。区内构造极为发育,区内的含矿蚀变带及石英脉与北西向构造关系密切。研究发现蚀变带、地表铁铜铅锌氧化物、石英脉是区内的找矿标志。
HeLuojia mining area in Dulan County-Qinghai Province are mainly looking for gold-polymetallic minerals,The mining area is located in HaTu gou area in the Middle Part of East KunLun,Between the Kunzhong Kunnan fault.The structure of the area is very well developed,The ore-bearing alteration zones and quartz veins in the area are closely related to the NW-trending structure.It was found that the alteration zone,Surface iron-copper-lead-zinc oxide and Quartz vein are the prospecting indicators in the area.
作者
赵立志
何利
李生虎
ZHAO Li-zhi;He Li;LI Sheng-hu(Qinghai No.5 Geological Exploration Institute,Xi'ning 810099,China)
出处
《世界有色金属》
2020年第17期64-66,69,共4页
World Nonferrous Metals
关键词
构造
热液脉型
金多金属矿
找矿潜力
Structure
Hydrothermal Vein Type
Gold polymetallic minerals
Prospecting potential