摘要
双山子铜多金属矿所出露地层应属大石寨组上段,安山岩、玄武岩形成较早,凝灰质砂砾岩、变质凝灰质砂岩形成较晚。矿(化)体多呈脉状产出,矿石以细脉状、浸染状及团块状为主,主要产于构造断裂中。
The strata exposed in Shuangshanzi copper polymetallic deposit belong to the upper Dashizhai Formation,andesite and basalt formed earlier,tuffaceous sand conglomerate and metamorphic tuffaceous sandstone formed later.Ore bodies are mostly vein-like.Ores are mainly veinlet,disseminated and mass-like,mainly occurring in structural faults.
作者
张化鹏
郎鹏林
朱健勇
高超
孙耀超
ZHANG Hua-peng;LANG Peng-lin;ZHU Jian-yong;GAO Chao;SUN Yao-chao(Inner Mongolia Shanjin Geological and Mineral Exploration Co.,Ltd.,Chifeng 024006,China)
出处
《世界有色金属》
2019年第14期253-253,255,共2页
World Nonferrous Metals
关键词
铅锌矿
EH4连续电导率测量
双山子
内蒙古
lead-zinc ore
EH4 continuous conductivity measurement
Shuangshanzi
Inner Mongolia
