{"title":"西非布基纳法索埃塞坎金矿床地质特征及找矿方向浅析","authors":"辉 靳","doi":"10.36012/se.v1i2.897","DOIUrl":null,"url":null,"abstract":"西非埃塞坎金矿床是一个石英碳酸盐网脉状矿床,赋存于砂岩和泥岩的褶皱浊积岩序列。高品位矿石多数产出于背斜轴部和东翼的层间部位,背斜东翼矿体沿倾向尚未封闭,矿体西翼尚未投入探矿工程,这将是下一步找矿工作的两个重点方向。","PeriodicalId":276517,"journal":{"name":"测绘与勘探","volume":"21 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-12-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"测绘与勘探","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.36012/se.v1i2.897","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
西非布基纳法索埃塞坎金矿床地质特征及找矿方向浅析
西非埃塞坎金矿床是一个石英碳酸盐网脉状矿床,赋存于砂岩和泥岩的褶皱浊积岩序列。高品位矿石多数产出于背斜轴部和东翼的层间部位,背斜东翼矿体沿倾向尚未封闭,矿体西翼尚未投入探矿工程,这将是下一步找矿工作的两个重点方向。
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