摘要
内蒙古自治区古巴林左旗中段铅锌矿地质特征具有构造简单和品位高的特点,经过多年的开仓工作,发现该矿床为小型铅锌矿床,为热液充填交代性,在开发利用过程中,顺应构造控制,取得了很好的社会效益和经济效益。本文针对内蒙古自治区古巴林左旗中段铅锌矿地质成因等进行分析和论证,能够有针对性地提出进行矿区开采的相关策略。
The geological characteristics of the lead-zinc deposit in the middle section of Linzuoqi,Inner Mongolia Autonomous Region,China,has the characteristics of simple structure and high grade.After many years of opening work,it is found that the deposit is a small lead-zinc deposit,which is hydrothermally filled and replaced.In the process,it conforms to the structural control and has achieved good social and economic benefits.This paper analyzes and demonstrates the geological genesis of the lead-zinc deposit in the middle section of Linzuoqi,Inner Mongolia Autonomous Region,and can propose relevant strategies for mining in a targeted manner.
作者
朱健勇
齐松
ZHU Jian-yong;QI Song(Inner Mongolia Shanjin Geology and Mineral Exploration Co.,Ltd.,Chifeng 024006,China)
出处
《世界有色金属》
2019年第9期125-125,128,共2页
World Nonferrous Metals
关键词
铅锌矿
地质特征
成矿原因
lead-zinc deposit
geological characteristics
metallogenic reasons