摘要
斑红山地区是青海省金银多金属矿的重要成矿区之一,大地构造属柴达木陆块,地处阿尔金山南坡,与柴达木盆地相接,俄博梁华力西期(钨、铋、稀土)成矿带使矿区的主要的分布地带。区内岩浆活动频繁,侵入岩广泛分布,NEE、近EW和近SN向断裂构造发育,该区成矿条件优越,具有寻找金(银)多金属矿的良好前景。
The spot in Hongshan area is one of the important metallogenic zone of Qinghai gold and silver polymetallic ore,the tectonic is Qaidam continental block,located in the southern slope,connected with the Qaidam Basin,the Variscan period OBO Liang（tungsten,bismuth and rare earth） metallogenic belt are the main distribution area of mining area.The magmatic activities in the area are frequent,and the intrusive rocks are widely distributed.NEE,near EW and near SN trending faults are developed.The metallogenic condition of the area is superior,and it has a good prospect for gold（silver） polymetallic deposits.
出处
《世界有色金属》
2017年第13期100-100,102,共2页
World Nonferrous Metals
基金
国土资源部公益性行业科研专项经费项目(编号:201411025)
柴达木盆地南北缘成矿系统与勘查开发示范项目(项目编号:2016-SF-A3)联合资助
关键词
斑红山地区
金银多金属矿
找矿探讨
Hongshan District
gold silver polymetallic ore
prospecting
