American Mineralogist · 2000 · 53 citations · 14 references
Natural SciencesMaterials EngineeringMaterials ScienceCrystal StructureInorganic ChemistrySolid-state ChemistryAluminum OxidesCrystal LatticeCrystal SymmetryCrystallographyX-ray CrystallographyX-ray DiffractionChainsCrystal Structure RefinementHigh-pressure Mineral PhasesPowder DiffractionPowder Diffraction AnalysisPowder X-ray DiffractionRietveld AnalysisRietveld Refinement
The crystal structure of CaMg2Al6O12, a new high-pressure phase synthesized at 21.8 GPa and 1200 °C using a multi-anvil apparatus, was solved by a newly developed structure program and refined by Rietveld analysis of the powder X-ray diffraction profile. The structure is hexagonal with cell constants a = 8.7616(2) and c = 2.7850(1) Å, and space group P63/m. The structure of this phase contains double chains of edge shared AlO6 octahedra running along the c axis. Three double chains share corners to form sixfold positions in which octahedrally coordinated Mg atoms reside. The large 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
14
Ionic radii for use in geochemistry
E. J. W. Whittaker, R. Muntus · Geochimica et Cosmochimica Acta · 1970 · 504 citations
The fate of subducted basaltic crust in the Earth's lower mantle
Kei Hirose, Yingwei Fei, Yanzhang Ma et al. · Nature · 1999 · 459 citations
Absence of an aluminous phase in the upper part of the Earth's lower mantle
Tetsuo Irifune · Nature · 1994 · 349 citations