文章摘要
李亚非.山西砖窑沟矿区冶镁白云岩矿床特征[J].矿产勘查,2018,9(6):1212-1216
山西砖窑沟矿区冶镁白云岩矿床特征
Characteristics of metallurical magnesium dolomite deposit in Zhuanyaogou mine area,Shanxi
投稿时间:2018-01-17  
DOI:
中文关键词: 岢岚县  冶镁白云岩  矿床特征  山西
英文关键词: kelan county, metallurical magnesium dolomite, deposit characteristics,Shanxi
基金项目:
作者单位
李亚非 山西地宝能源有限公司, 太原 030045 
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中文摘要:
      山西省岢岚县砖窑沟矿区冶镁白云岩矿位于岚漪镇砖窑沟村一带,所在区域为吕梁山北段。该区域分布大面积沉积地层,地层多为单斜构造。区内断层构造较少,主要有北西向断层和北东东向断层。冶镁白云岩矿体赋存于该区域沉积岩地层中,利用科学有效的地质工作手段及方法,通过仔细深入的研究,认识到矿体的形态特征、矿床特征以及地层构造特征。区内整体为一单斜构造,该矿床为原生沉积矿床后期受断层影响,矿床内部存在小褶曲为单斜构造。
英文摘要:
      The metallurical magnesium dolomite deposit is located in Zhuanyaogou village of Lanyi town, in Kelan county, Shanxi. The study area is the north part of Luliang mountain. In this area, there is a large area of sedimentary formation, mostly appearing as monocline. There are a few of faults structures in the region, mainly are NW and NEE faults. Metallurigcal magnesium dolomite ore bodies occur in the sedimentary strata. This paper conducted geological work in scientific and effective means and methods, through careful research, made clear understanding about the morphological characteristics of the ore bodies, ore deposit features and the characteristics of strata structure. The whole area is a monocline and the deposit is a single oblique tectonic deposit with small folds in it.
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