摘要
双鱼山金矿是新疆东天山地区新发现金矿,赋矿围岩为浅变质的雅满苏组,为一套沉积细碎屑岩建造和火山岩建造。金矿化受构造及岩体联合控制,主成矿期发生于脉岩形成后的构造破碎及岩石蚀变阶段,矿床为构造蚀变岩型金矿床。
Shuangyushan gold deposit is a newly discovered one in the East Tianshan area of Xinjiang.The host rock is a light metamorphosed Yamansu formation,It is a set of sedimentary fine clastic rock formation and volcanic rock formation.Mineralization is jointly controlled by structure and rock mass.The main ore-forming period occurs in the stage of structural fracture and rock alteration after the formation of vein rock.The deposit is a structural altered rock type gold deposit.
作者
班建永
付清波
BAN Jianyong;FU Qingbo(The First Regional Geological Survey Team of Xinjiang Bureau of Geo-exploration and Mineral Development,Urumqi 830011,China)
出处
《四川有色金属》
2020年第2期24-26,共3页
Sichuan Nonferrous Metals
关键词
双鱼山金矿
地质特征
构造蚀变岩型
成矿化学特征
Shuangyushan gold deposit
geological characteristics
structural altered rock type
metallogenic chemical characteristics