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新疆哈密双鱼山金矿地质特征及成因分析

Geological Characteristics And Genetic Analysis Of Shuangyushan Gold Deposit,Hami,Xinjiang
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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
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