摘要
小秦岭金矿田主要位于华北地台南缘陕西潼关、河南灵宝一带,秦岭造山带为主要成矿构造带;石英脉型金矿为主要成矿类型,特别是第Ⅱ石英—黄铁矿阶段和第Ⅲ石英—多金属硫化物阶段为金矿主要成矿阶段,在小秦岭地区找矿具有指导意义。
The small Qinling Gold fields are mainly located at Tongguan, Henan Lingbao area in the Tainan margin of north China, and the Qinling orogenic belt as the main metallogenic tectonic belt;the quartz vein type gold deposit is the main metallogenic type, especially the Ⅱ quartz-pyrite stage and the Ⅲ quartz-polymetallic sulfide phase as the main metallogenic stage of gold deposit, which is instructive in the small qinling region.
作者
徐宪立
张剑锋
XU Xian-li;ZHANG Jian-feng(Henan nonferrous Geology and Minerals Bureau Sixth Geological Brigade,Zhengzhou 450016,China;Henan Golden Channel Gold Co., Ltd., Sanmenxia 472000,China)
出处
《世界有色金属》
2019年第3期266-268,共3页
World Nonferrous Metals
关键词
地质特征
成矿阶段
研究意义
含金石英脉
geological characteristics
metallogenic stage
research significance
quartz veins containing gold