摘要
日吉普金多金属矿位于黑山—祁曼塔格成矿远景区西部,赋存于石炭系喀拉米兰河群,受北西向韧脆性断裂控制,发现的两条金多金属矿与北西向韧脆性断裂方向一致。
Rijipu gold-bearing polymettalic deposit is located in the west part of the Heishan-Qi- mantage mineralization prospect area. It occurs in the Carboniferous Kalamilanhe Group and is controlled by ductile-brittle faults at northwest trend. Two gold-bearing polymettalic zones are discovered to be in a similar direction with the northwest ductile-britde faults.
出处
《陕西地质》
2015年第1期29-33,共5页
Geology of Shaanxi
关键词
东昆仑地区
金多金属矿
地质特征
控矿因素
East KunIun area
polymettalic ore
geological features
ore-controlled factors
