In more acid environments, as in the Dystropept, the plagioclases alter to metahalloysite and some amorphous aluminosilicates, and the augite to amorphous iron hydrous-oxide and goethite. In a freely drained environment as in the Tropudult, the alteration of plagioclases leads to kaolinite and locally to gibbsite; all the augite is converted to ...
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