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Figure 4
(a) The structure of BPO4 ([I\bar 4]) at 6.1 GPa, projected on the ab plane. It is cristobalite-like and, under pressure, undergoes a continuous tilting of the B(P)O4 tetrahedra up to collapse, at 50 GPa, into an almost regular f.c.c. array of the O atoms represented in (b). This final step corresponds to the chalcopyrite structure of CuFeS2. Note that the rhombs seen in (a) are equivalent to those described in Fig. 2[link](a). In this continuous tilting of tetrahedra, the cation array BP remains as a blende-type structure.

Journal logoSTRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS
ISSN: 2052-5206
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