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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Geochemistry of a sedimentary lateritic kaolin deposit in Quadrilatero Ferrifero,Brazil
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Geochemistry of a sedimentary lateritic kaolin deposit in Quadrilatero Ferrifero,Brazil

机译:巴西Quadrilatero Ferrifero的沉积红土高岭土矿床的地球化学

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摘要

The present study deals with the mineralogy and geochemistry of the clayey facies of the Agua Limpa kaolin deposit,situated in the Moeda Syncline,Quadrilatero Ferrifero,Minas Gerais,Brazil.Kaolinite,quartz,oxides and iron hydroxides (hematite and goethite) represent the mineral assembly of the five facies of the deposit.White mica,rutile,anatase and gibbsite are heteroge-neously distributed along the profile.Despite the variable behavior of the chemical elements along the profile,the geochemical patterns for major and rare earth elements enable to define the filiations generated by the laterization process that affected the sediments.
机译:本研究涉及位于Moeda Syncline,Quadrilatero Ferrifero,Minas Gerais,巴西的Agua Limpa高岭土矿床的黏土相的矿物学和地球化学。高岭石,石英,氧化物和氢氧化铁(赤铁矿和针铁矿)代表矿物矿床五个相的集合。白云母,金红石,锐钛矿和三水铝石沿剖面异质分布。尽管化学元素沿剖面的行为各异,但主要和稀土元素的地球化学模式却可以确定后期沉积过程中产生的影响沉积物的纤维化。

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