摘要
英德白水寨钨多金属矿位于粤北钨多金属成矿带的雪山嶂矿田内。与典型的石英脉型黑钨矿相比,该矿床具有浅部细网-细脉带钨矿物“上白下黑”、发育细网脉与矽卡岩化叠加的白钨矿(化)体、矿石矿物组合中出现大量黄铁矿的独特特征。目前揭露的地表-浅部还处于“五层楼”模式的细网脉标志带-细脉带位置,矿区深部找矿空间大。
Yingde baishuizhai tungsten polymetallic deposit is located in xuesshanzhang ore field of north guangdong tungsten polymetallic metallogenic belt.Compared with the typical quartz vein type wolframite,the deposit has the unique characteristics of"upper baibai lower hei"tungsten mineral in the finette-veinlets zone,the scheelite(mineralization)bodies superimposed by the development of finette-veinlets and skarnization,and a large amount of pyrite in the mineral assemblage.At present,the exposed surface-shallow part is still in the"five-storey"mode of fine mesh vein marker belt-veinbelt location,deep mining exploration space.
作者
李春武
LI Chun-wu(guangdong institute of nonferrous geology,Guangzhou 510050,China)
出处
《世界有色金属》
2019年第8期112-112,114,共2页
World Nonferrous Metals
关键词
石英脉型
地质特征
成矿模式
Quartz vein type
Geological features
Metallogenic model
