红土式风化作用导致四种元素成矿,即:铁、铝、镍和锰。广泛一致的看法是,红土式矿石的生成主要归因于相对的富集,也就是说:易溶解的组分如硅酸、碱、碱土元素的浸出,导致难溶组分残留富集起来。 Lateritic weathering led to the formation of four elements, namely iron, aluminum, nickel and manganese. It is widely agreed that the production of lateritic ores is mainly due to relative enrichment, that is to say, the leaching of easily soluble components such as silicic acid, alkali and alkaline earth elements leads to enrichment of the insoluble components.