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来自维基百科,自由的百科全书
铁石是一种含铁不少于15%的沉积岩,可以为直接沉积,也可为化学交代而产生。这一术语习惯用来描述前寒武纪之后的条带、非条带、非黏土沉积岩。前寒武纪的铁建造(iron formation)具有不同起源,一般称为條狀鐵層。铁石的组成可以是氧化物,如:褐铁矿、赤铁矿、磁铁矿;碳酸盐,如菱铁矿;硅酸盐,如鲕绿泥石;或者它们的组合。[1][2]
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