摘要
中非铜矿带是世界上最主要的沉积型铜-钴矿成矿带之一,赞比亚铜矿带是其重要组成部分,其内有沉积型铜矿、热液脉型铜矿和变质热液型铜矿,矿床受地层、岩相、古地理环境和构造的控制。
The central African copperbelt is one of the most important sedimentary copper-cobalt metallogenic belts in the world,Zambia copperbelt is an important part of it,which include sedimentary type,hydrothermal vein type and metamorphic hydrothermal type copper deposits that are controlled by stratum,lithofacies,paleogeographical environment and structure.
作者
周聪
ZHOU Cong(Sinomine Resource Exploration Co.,Ltd.,Beijing 100089,China)
出处
《世界有色金属》
2018年第10期150-151,共2页
World Nonferrous Metals
关键词
赞比亚铜矿带
地质特征
控矿因素
Zambia copperbelt
geological features
ore-controlling factors