In order to test the possible dynamical origin of the incommensurate phase of quartz, the dispersion of low-energy phonon branches in high quartz has been determined by inelastic neutron scattering. The optical sof tmode associated with the α-β transition and the transverse acoustic mode corresponding to u xy strains exhibit a large anisotropy within the hexagonal plane. The relations of these results to the phenomenological gradient coupling model and to microscopic lattice dynamical models are discussed.
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Bethke et al. (1987) studied this question.
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