摘要
在日沟铜铅多金属矿地表矿体均产于上三叠统陆相火山岩中,受断裂构造、火山构造控制明显,Cu、Mo、W、Sn、Pb、Zn、Ag等元素在平面上具明显的分带性,深部矿体在火山岩中、变质杂岩体中均有发育。通过对矿区内地层、构造特征、岩浆活动、矿化蚀变等现象以及多年的找矿成果分析,矿床类型为斑岩型矿床,具有良好的找矿前景。
The surface orebodies of copper and lead polymetallic ore in the day trench are all produced in the continental volcanic rocks of the Upper Triassic, and controlled by fault and volcanic structures Visibility. Cu, Mo, W, Sn, Pb, Zn and Ag are divided in plane and the deep orebodies are developed in volcanic rocks and Metamorphic rocks. Based on the analysis of strata, tectonic features, magmatic activity, mineralization alteration and ore prospecting results in the mining area, the type of deposit is Porphyry type and there is a fine prospect of ore prospecting, .
作者
范国均
贺淑兰
杜海斌
FAN Guo-jun;HE Shu-lan;DU Hai-bin(Tibetan institute of Nuclear Geology, Chengdu 610052, China)
出处
《世界有色金属》
2018年第3期140-141,共2页
World Nonferrous Metals
关键词
铜钼多金属矿
杂岩体
在日沟
火山穹隆构造
成矿模式
Copper lead polymetallic ore
Miscellaneous rock mass
Zairigou
Volcanic dome structure
metallogenic patterns