摘要
葡萄溪地区铅锌矿矿床成因类型为岩浆热液充填脉状矿床,受NWW向断裂控制。含矿地层主要为奥陶系黄隘组板岩夹粉砂质板岩、含钙质板岩等。
The genesis of the lead-zinc deposit in the grapevine area is a magmatic hydrothermal filling vein deposit,controlled by the NWW fault.The ore bearing strata are mainly Ordovician yellow pass group slate,silty slate,calcareous slate and so on.
作者
周荣幸
刘春丽
ZHOU Rong-xing;LIU Chun-li(The Guangxi Zhuang Autonomous Region Geological Survey Institute,Nanning 530023,China)
出处
《世界有色金属》
2018年第11期143-144,共2页
World Nonferrous Metals
关键词
葡萄溪地区
铅锌矿
地质特征
成矿规律
grapevine area
lead-zinc deposit
geological characteristics
metallogenic regularity
