摘要
工作区位于青海省西南部,柴达木盆地东南,隶属青海省玉树藏族自治州曲麻莱县管辖。距离曲麻莱县约45 km,道路泥泞颠簸,交通条件较差。工作区位于巴颜喀拉断陷盆地及其中的三叠纪、古近纪-新近纪、第四纪地层。在此,该文将针对该多金属矿对应的地质特征以及相关成因进行简要探讨。
The working area is located in the southwest of Qinghai Province and the southeast of Qaidam Basin, and it is under the jurisdiction of Qumalai County, Yushu Tibetan Autonomous Prefecture, Qinghai Province. It is about 45km away from Qumalai County. The road is muddy and bumpy, and the traffic conditions are poor. The working area is located in Bayan Karla fault depression basin and its middle Triassic, Paleo-Neocene and Quaternary strata. In this paper, the corresponding geological characteristics and related genesis of the polymetallic ore are briefly discussed.
作者
高建会
Gao Jianhui(Beijing Simon mineral exploration co.LTD,Beijing 100000,China)
出处
《有色金属设计》
2018年第3期60-63,共4页
Nonferrous Metals Design
关键词
地层
构造
岩浆活动
变质作用
矿化蚀变
Stratum
Structure
Magmatic activity
Metamorphism
Mineralized alteration