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Depending on the sequence of tetrahedral (T) and octahedral (O) sheets, clay minerals can be classified and designed as 1:1 or TO and 2:1 or TOT phyllosilicates. Representative examples of 1:1 phyllosilicates are kaolinite (Al silicate) and serpentine (Mg silicate). This chapter presents an overview of the field of hybrid materials based on the intercalation of organic species into 2D silicates, which...
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