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The title compound is closely related to InFeO3, consisting of alternating layers of InO6 octahedra and FeO5 trigonal bipyramids. According to substitution of Ti4+ for Fe3+, excess O atoms are introduced into the Fe-O trigonal lattice plane of InFeO3.
Supporting information
| Crystallographic Information File (CIF) Contains datablocks global, 1 |
| Structure factor file (CIF format) Supplementary material |
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