A corrugated [Si2O2N2]2− layer anion, which is constructed of dreier rings, forms the basis of the silicate Ca[Si2O2N2] (see picture). The unusual structure results from the fact that every N atom—unlike the O atoms in oxosilicates—links three neighboring Si tetrahedron centers within the layers, whereas all the O atoms are exclusively bonded terminally to the Si atoms.
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Höppe et al. (2004) studied this question.
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