摘要
查涌铜多金属矿处于三江成矿带北西段,成矿地质背景较好。在综合对比矿床宏观、微观成矿特征的基础上,结合矿区勘查工作进展,对矿床的成矿规律、找矿标志、成因及找矿前景进行了初步分析,认为该区成矿热液可能由深部隐伏岩体引起,深部具有寻找岩浆热液型铜钼多金属矿的潜力。
The copper polymetallic ore deposit is in the north western section of the sanjiang metallogenic belt, and the geological background is better. In comprehensive comparing metallogenic characteristics on the basis of macro and micro, combined with the mining exploration work, the metallogenic regularity of ore deposit and prospecting marks, genesis and prospecting prospect has carried on the preliminary analysis, thought the ore-forming hydrothermal may be caused by the deep concealed rock mass, deep is looking for magmatic hydrothermal type copper molybdenum polymetallic ore potential.
出处
《世界有色金属》
2017年第15期136-139,共4页
World Nonferrous Metals
关键词
成矿地质特征
矿床成因
查涌铜多金属矿
青海治多县
Ore-forming geological characteristics
Ore deposit genesis
Check surge copper polymetallic deposits
For manycounty in qinghai