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首页> 外文期刊>Journal of Mining and Geology >Mineralogy and geochemistry of lateritic weathering profiles on ultramafic rock bodies around Mokuro in Ile-Ife area, southwestern Nigeria
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Mineralogy and geochemistry of lateritic weathering profiles on ultramafic rock bodies around Mokuro in Ile-Ife area, southwestern Nigeria

机译:尼日利亚西南部Ile-Ife地区Mokuro附近超镁铁质岩体的红土风化剖面的矿物学和地球化学

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摘要

Two laterite profiles on ultramafic rocks in Mokuro-Ife area of southwestern Nigeria, were investigated for the formation of secondary minerals and trace element behavior during humid tropical weathering. Microscopic and X-ray data indicate that the rocks alter to talc, tremolite and chromiferous chlorite. Chlorite becomes thre major stable component and is concentrated in the weathering profile. Geochemical data further indicated that with increasing depth, Fe_2O_3 and Al_2O_3 contents decrease, whereas SiO_2 and MgO increase. Trace elements such as Ni, Co, Cr, Mn and Cu are all concentrated in the lattice of goethite. Comparison with data on soils overlying associated metapelitic schist shows that geochemical investigation on residual soil may be used for mapping purposes in area with thick weathering overprint.
机译:研究了尼日利亚西南部Mokuro-Ife地区超镁铁质岩石上的两个红土剖面,研究了潮湿热带风化过程中次生矿物的形成和微量元素的行为。显微和X射线数据表明,这些岩石变为滑石,透闪石和亚铬绿亚氯酸盐。亚氯酸盐成为主要的稳定成分,并集中在风化剖面中。地球化学数据进一步表明,随着深度的增加,Fe_2O_3和Al_2O_3的含量减少,而SiO_2和MgO的增加。镍,钴,铬,锰和铜等微量元素都集中在针铁矿晶格中。与覆盖在相关变质岩片岩上的土壤数据的比较表明,对残留土壤的地球化学研究可用于风化叠印较厚的地区的测绘目的。

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