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Figure 5
Evidence of the splitting of reflections in the (hk0) plane, arising from the presence of new ferroelastic domains derived from the loss of a glide plane perpendicular to amon in the phase transition P21/b11 [\rightarrow] P[\bar 1]. (a) Reflection (330)mon at 293 K, before the phase transition. (b) Same reflection (600)tric at 180 K, where the splitting in two is obvious. (c) and (d) represent the same for reflections (3[\bar 7]0)mon and [(6 \bar{10} 0)_{\rm tric}], respectively.

Journal logoSTRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS
ISSN: 2052-5206
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