摘要
金及多金属矿化破碎蚀变带与逆断层关系密切,柱状、针状白色毒砂及细微粒黄铁矿是金的重要标志性矿物,成矿带具有良好的成矿地球化学背景和成矿地质条件,良好的控矿、容矿构造条件。
The Au and multimetallic metallogenesis fracture alteration zone is in the close relation with the thrust. The columnar, needle- like white arsenopyrite and fine -micrograined pyrite are the important indicator minerals of gold. The metallogenetic zone has not only the good geochemical background and geological condition of metallogenesis but also good structure condition of ore control, ore bearing and ore prospecting potentiality.
出处
《云南地质》
2011年第1期22-24,27,共4页
Yunnan Geology
关键词
粒间—裂隙金
针状白色毒砂
细微粒黄铁矿
重要标型矿物
青海大柳沟金矿
Intergranular - Fissure Au
Needle - Like White Arsenopyrite
Fine - Micrograined Pyrite
Important Typomorphic Mineral
Daliugou Au Deposit, Qinghai
