摘要
锑才克巴依金矿是东准噶尔地区发现的破碎带蚀变岩型金矿。该矿产于陆缘火山岩浆弧区,成因与强应变构造带及浅成、超浅成岩脉有关,成矿流体为高温近中性溶液,矿体受断裂破碎带控制。
Dicaikebayi gold deposit is of alteration type discovered in the fracture zones of east Junggar region. The deposit occurs at volcanomagmatic arc regions of continental margin, genetically related with high-strained structural zones and hybabyssal-uhrabyssal veins. The metallogenic is nearly intermediate high-temperature solution. The ore body is controlled by fracture zones.
出处
《四川有色金属》
2015年第3期40-43,共4页
Sichuan Nonferrous Metals
关键词
锑才克巴依金矿
地质特征
成因探讨
Dicaikebayi gold deposit
geological characteristics
discussions for genesis
