Figure 4
(a) The structure of BPO4 ( ) 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 (a). In this continuous tilting of tetrahedra, the cation array BP remains as a blende-type structure. |