Clay Mineral, Kaolin-serpentine group
Minerals of this groups are 1:1 layer silicates. Their basic unit of structure consists of tetrahedral and octahedral sheets in which the anions at the exposed surface of the octahedral sheet are hydroxyls (see Figure 4). The general structural formula may be expressed by Y2 - 3Z2O5(OH)4, where Y are cations in the octahedral sheet such as Al3+ and Fe3+ for dioctahedral species and Mg2+,
posted by SuddenCat @ 10:34 PM
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