摘要
青海大格勒东金多金属矿矿区位于柴达木盆地南缘,构造带内岩浆侵入活动极为强烈,断裂构造和侵入岩体是区内成矿和控矿的主要因素。通过矿区的地质特征、矿体特征的分析,对找矿前景进行了预测。
The Gold polymetallic ore deposit in Dagledong of Qinghai province is located in the south margin of Qaidam Basin.The magmatic intrusion in the structural belt is very strong.The fault structure and intrusive rock body are the main factors for mineralization and ore control in the area.Based on the analysis of the geological characteristics and orebody characteristics of the mining area,we think that the prospecting prospect is predicted.
作者
张学德
陈万龙
马维明
王振东
马英
罗永统
ZHANG Xuede;CHEN Wanlong;MA Weiming;WANG Zhendong;MA Ying;LUO Yongtong(College of Earth Science, Jilin University, Changchun, Jilin 130000, China;Qinghai Geological Survey Bureau, Xining, Qinghai 810000, China;No. 7 Team, Qinghai Bureau of Nonferrous Geology and Mineral Exploration, Xining, Qinghai 810000, China)
出处
《中国锰业》
2020年第3期16-19,共4页
China Manganese Industry
基金
青海省有色地质矿产勘查局基金项目([2016]160号)。
关键词
金多金属矿
地质特征
矿体特征
找矿前景
Gold polymetallic ore
Geological features
Characteristics of ore body
Prospecting prospect
