Differential scanning calorimetry on powders and x-ray diffraction on singl
e crystals of (CH3)(4)NSCN reveal a cell-doubling cubic-to-orthorhumbic (O-
h(1)-->D-2h(13)) ferroelastic transition at 181 degrees C. This transformat
ion is interpreted as a two-step mechanism in which an incomplete ordering
of the SCN groups triggers the ferroelastic deformation, ia an intermediate
tetragonal or orthorhombic phase. Diffuse scattering and diffraction patte
rns under stress illustrate the theoretical argumentation. [S0163-1819(99)1
4421-7].