新疆金龙山金矿床地质特征及其成矿化学特征分析  

Geological characteristics and metallogenic chemical characteristics of Jinlongshan gold deposit, Xinjiang

作　　者：班建永[1] BAN Jian-yong(The first regional geological survey team of Xinjiang Uygur Autonomous Region Bureau of Geology and mineral exploration and development,Urumqi 830011,China)

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第一区域地质调查大队,新疆乌鲁木齐830011

出　　处：《世界有色金属》2020年第3期102-103,共2页World Nonferrous Metals

摘　　要：新疆金龙山金矿属于韧性剪切破碎蚀变岩型金矿,大地构造处于觉罗塔格裂陷槽之雅满苏裂谷,韧性剪切带为矿区主要控矿构造,区域沉积建造浅变质的细碎屑岩建造和火山岩建造,异常元素一般为Au、As、Sb、Cu、Mo、Pb、Zn。Jinlongshan gold deposit in Xinjiang belongs to the ductile shear fracture altered rock type gold deposit.The geotectonics is located in Yamansu rift of juelutage rift.The ductile shear zone is the main ore controlling structure of the mining area.The regional sedimentary formation is light metamorphosed fine clastic rock formation and volcanic rock formation.The abnormal elements are generally Au,as,Sb,Cu,Mo,Pb,Zn.

关 键 词：金龙山金矿 地质特征 成矿化学特征 

分 类 号：P618.51[天文地球—矿床学]