山西省闻喜县刘庄冶矿区铜矿地质特征研究  

Study on the Geological Characteristics of Copper Deposits in Liuzhuangye Mining Area,Wenxi County,Shanxi Province

作　　者：邓婧 DENG Jing(Shanxi Provincial Geological Survey Bureau 214 Geological Team Co.,Ltd,Yuncheng 044000,China)

机构地区：[1]山西省地质勘查局二一四地质队有限公司,山西运城044000

出　　处：《世界有色金属》2023年第12期99-101,共3页World Nonferrous Metals

摘　　要：刘庄冶矿区铜矿分布于山西省闻喜县境内,位于胡家峪—上玉坡短袖背斜南东翼,区内褶皱构造发育,为铜矿成矿创造了有利条件。目前矿区内已探明大小铜矿体48条,矿体均呈透镜状、扁豆状产出于篦子沟组黑色片岩和余家山组厚层大理岩的接触带中,顶底板围岩主要为大理岩和黑色片岩。结合前人针对矿区开展过大量的地质研究资料表明,矿区找矿潜力较大,具有较好的开发利用前景。基于此,本文在全面收集以往地质资料基础上对矿区铜矿地质特征进行系统研究,以期能为当地同类型的铜矿成矿条件和成矿规律的研究提供一些有益参考。The copper deposits in Liuzhuang Metallurgical Mining Area are distributed in Wenxi County,Shanxi Province,and are located in the southeast wing of Hujiayu Shangyupo short sleeve anticline.The development of fold structures in the area creates favorable conditions for copper mineralization.At present,48 large and small copper ore bodies have been proved in the mining area.The ore bodies are lenticular and lenticular and occur in the contact zone of black schist of Bizigou Formation and thick marble of Yujiashan Formation.The roof and floor wall rocks are mainly marble and black schist.Combined with a large number of geological research data carried out for the mining area by predecessors,it shows that the mining area has great prospecting potential and good development and utilization prospects.Based on this,this paper conducts a systematic study on the geological characteristics of copper deposits in the mining area on the basis of comprehensive collection of previous geological data,hoping to provide some useful references for the study of local copper ore forming conditions and laws of the same type.

关 键 词：刘庄冶矿区 铜矿地质特征 山西省闻喜县 

分 类 号：P618.41[天文地球—矿床学]