摘要
山西省铅锌矿产资源较为匮乏,可供开发利用的矿产地分布较少,主要集中分布于山西五台山-恒山一带的灵丘太白维山地区。成矿时代主要为中生代燕山期,断裂构造系统可作为良好的导矿构造和储矿构造,在中低温条件下含矿热液发生交代充填作用,形成各种与铅锌共-伴生的多金属矿床。
The lead and zinc mineral resources in Shanxi Province are relatively scarce,and the mineral resources available for exploitation and utilization are less distributed,mainly concentrated in Lingqiu Taibaiwei Mountain area in Wutai Mountain-Hengshan area of Shanxi Province.The metallogenic epoch is mainly the Mesozoic Yanshanian epoch.The fault tectonic system can be used as a good ore-conducting structure and ore-storing structure.Metasomatic filling of ore-bearing hydrothermal fluids occurs under the conditions of medium and low temperature,forming various polymetallic deposits associated with lead and zinc.
作者
黄晋荣
HUANG Jin-rong(Shanxi Institute of Geological Survey,Taiyuan 030006,China)
出处
《世界有色金属》
2019年第15期80-81,共2页
World Nonferrous Metals
关键词
典型矿床
多金属共-伴生
断裂构造
typical deposits
polymetallic co-occurrence
fault structure
