“…After the structurally inhomogeneous phase in MgBF 6 •6H 2 O (B = Si, Ge, Ti) crystals, existing between their rhombohedral paraelastic phase and their monoclinic ferroelastic one, had been discovered by Ziatdinov et al [12][13][14][15], most of the attention of interested researchers [12][13][14][15][17][18][19][20][21][22][23][24][25] was attracted to the nature of this phase (hereafter in this paper called the 'intermediate' phase). For the interpretation of experimental data, various different models of the 'intermediate' phase in these crystals have been suggested: some modifications of the incommensurate structure model [12][13][14][15][17][18][19][20][21][22], a model of static and dynamic disordered structure fragments [23,24] and the domain model [25]. All of these models have been analysed by us previously, with application to MgSiF 6 •6H 2 O [42].…”