供稿: 袁杨森;高灶其;张成学;徐红伟 | 时间: 2018-12-28 | 次数: |
作者单位:河南省地质矿产勘查开发局第二地质队
摘要:根据在几内亚博凯地区Keveoul铝土矿勘探区所获得的部分地质勘探资料,对该地区红土型铝土矿成矿机理和控矿因素进行了分析.研究表明,其风化剖面大致分为3个特征带,从上至下分别是铁质壳、结核带和密高岭土带,矿石主要分布在铁质壳和结核带中.化学分析表明,铁铝化合物在结核带以上较为富集,二氧化硅在结核带以下含量较高,同时在风化壳的上部,铁-铝有着明显的分离过程,由此可以运用阶段说来探讨母岩通过地球化学元素迁移,最后形成铝土矿床的过程.同时就地貌、水文地质条件等控矿因素对矿床的影响进行了分析.
基金:河南国际合作(集团)有限公司几内亚共和国博凯地区558平方公里铝土矿勘查项目;
DOI:10.16186/j.cnki.1673-9787.2010.03.014
分类号:P618.45
Abstract:With the research on the geological data obtained from Keveoul exploration area of bauxite in Boke of Guinea, the ore forming mechanism and the ore controlling factors are analysed.Results show the weathering profiles are usually comprised of three main zones, which are duricrust, nuclear zone and saprolite from top to down.Ore mainly distributes in duricrust and nuclear zone.But chemical analysis indicates that Al and Fe compound is enriched upon the nuclear zone, and SiO2 contents is high below the nuclear zone.In the upside of weathering mantle, the separation of Al and Fe is obvious.So we can use the phases theory to discuss the process of the bauxite deposits forming by the parents rock migration through geochemical elements.In the meantime, the influence of physiognomy, hydrogeologic elements and so on upon the bauxite deposits is analyzed.
Keyword:lateritic bauxite deposits;weathering profiles;ore forming mechanism;ore controlling factors;