摘要
京根郭勒地区位于宗务隆山华力西期铅、银、铜、金成矿带。通过研究认为,矿体受北西-南东向构造控制,京根郭勒多金属矿成矿类型为含金-硫化物同构造脉型金矿矿床。指出矿区中已发现矿体的两端具有较好的找矿空间,下一步工作应针对矿体两端的化探异常区继续开展找矿工作,摸清矿体地表展布形态,争取该矿区找矿的更大突破。
The Jinggengguole area is located in the Zongwulong Mountain Hualixi Period Lead, silver, copper, gold mineralization belt.According to the study, the ore bodies are controlled by the northwest-southeast fault and abnormal shape.The type of Jinggeng- guole Multi-metal deposits gold-sulphide accompanied structure in type gold deposit. It is pointed out that the two ends of the ore body are prospecting space in the mine.The next step should keep to prospect for the geochemical exploration anomalies at both ends of the ore body and find out the distribution of the ore body on surface to achieve a greater breakthrough in the mine.
作者
付彦文
李良俊
杨海云
余福承
FU Yan-wen;LI Liang-jun;YANG Hai-yun;YU Fu-cheng(The northern Qinghai-Tibet plateau Geological Processes and Mineral Resources Laboratory,Xining 810012;Qinghai Institute of Geological Survey, Xining 810012;The third institute of Qinghai geological mineral prospecting,Xining 810000;The second institute of Qinghai geological mineral prospecting,Xining 810028)
出处
《矿产勘查》
2018年第4期559-563,共5页
Mineral Exploration
基金
青海省地质勘查基金项目资助
关键词
宗务隆
京根郭勒矿区
地质特征
金铅锌矿
Zongwulong
Jinggengguole area
geological characteristics
gold-lead-zinc deposit