摘要
本文通过系统整理临武县四一八铅锌矿地质成果资料,基于“三位一体”成矿模式,结合矿区地质特征认真分析矿床成因,总结矿区成矿规律,探讨矿区“底板成矿”理论指导边深部找矿预测的可能性,为矿山边深部找矿寻求新突破提供找矿线索,提高找矿精准度。
Based on the"Trinity"metallogenic model,combined with the geological characteristics of the mining area,this paper analyzes the genesis of the deposit,summarizes the metallogenic law of the mining area,and discusses the possibility of the"floor metallogenic"theory to guide the prospecting and prediction in the edge and deep parts of the mine,so as to provide prospecting clues and improve the prospecting efficiency Accuracy.
作者
胡雄成
HU Xiong-cheng(Team 408,Hunan Bureau of Geology and mineral exploration and development,Chenzhou 423000,China)
出处
《世界有色金属》
2021年第7期88-89,共2页
World Nonferrous Metals
关键词
铅锌矿
地质特征
矿床成因
临武
lead zinc deposit
geological characteristics
deposit genesis
Linwu