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Experiments in the system Mg 2 SiO 4 -Fe 2 SiO 4 -Fe 3 O 4 have produced three intermediate phases that are stable between ~4.0 and 9.0GPa and 1100 o C. These phases are different spinelloid polytypes and are structural analogues to spinelloids II, III and V in the Ni-aluminosilicate system [J. Solid State Chem. 44 (1982) 257]. The behaviour...
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