The crystal structure of CaMg2Al6O12, a new high-pressure phase synthesized
at 21.8 GPa and 1200 degreesC using a multi-anvil apparatus, was solved by
a newly developed structure program and refined by Rietveld analysis of th
e powder X-ray diffraction profile. The structure is hexagonal with cell co
nstants a = 8.7616(2) and c = 2.7850(1) Angstrom, and space group P6(3)/m.
The structure of this phase contains double chains of edge shared AlO6 octa
hedra running along the c axis. Three double chains share corners to form s
ixfold positions in which octahedrally coordinated Mg atoms reside. The lar
ge Ca atoms are randomly distributed at ninefold sites with half-occupancy
in the hexagonal tunnel. Previously reported Al-rich silicate phases could
possibly have the same structure. This structure could thus qualify as one
of the possible major host phases for aluminum in the lower mantle.