Acta Cryst. (2001). A57, 406-413 [ doi:10.1107/S0108767301003087 ]
Abstract: A phase transition between the diamond (
) and the lonsdaleite types (P63/mmc) may be described as a deformation of a homogeneous sphere packing with three contacts per sphere (type 3/10/o1) in the common subgroup Pnna of
and P63/mmc. The frequently observed transition between the zinc-blende (
) and the wurtzite types (P63mc) may be described in an analogous way as a deformation of a heterogeneous sphere packing in the subgroup Pna21. The proposed model guarantees the three-dimensional connection during the whole transformation process. By this property it is distinguished from other models.
Keywords: phase transitions; diamond-lonsdaleite; zinc-blende-wurtzite; tridymite-cristobalite; sphere packings.
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