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. |