The kaolin subgroup of layer silicate clay minerals includes halloysite, nacrite, dickite, kaolinite and odinite. Except for odinite and halloysite, these industrially essential minerals show the same chemical composition: Al2Si2O5(OH)4. Mainly formed by the weathering of feldspar and muscovite (for example, alteration of granitic rocks), kaolin minerals are prevalent in the sediments and soils of...


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July 1, 2024
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