Acta Cryst. (2002). A58, 327-333 [ doi:10.1107/S0108767302005287 ]
Abstract: A model was derived for the temperature-dependent phase transition between the high-temperature polymorphs of quartz (P6422) and tridymite (P63
mmc). Only the Si framework is considered, and the transformation can be described as a deformation of a homogeneous sphere packing with three contacts per sphere (type 3/10/h1) in the common subgroup P6122 of P6422 and P63
mmc. The proposed model guarantees the three-dimensional connection of the crystal structure during the whole transformation process.
Keywords: phase transitions; quartz; tridymite; sphere packings.
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