At last! The single-crystal X-ray structure of a naturally occurring sample of the ilmenite-type oxide FeCrO3

Pérez-Cruz, M.A.; Elizalde-González, M.P.; Escudero, R.; Bernès, S.; Silva-González, R.; Reyes-Ortega, Y.

doi:10.1107/S2052520615015838

Acta Crystallographica Section B
Acta Crystallographica
Section B STRUCTURAL SCIENCE, CRYSTAL ENGINEERING AND MATERIALS

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Figure 4
ORTEP-like view for face-sharing [CrO₆] and [FeO₆] octahedra with 99% probability level displacement ellipsoids. Atoms Cr1, O1 and Fe2 constitute the asymmetric unit, and other O atoms are generated by symmetry codes: (i) y, x-y, z; (ii) -y, -x, z; (iii) $[-x + {1\over 3}, -y - {1\over 3}, -z + {2\over 3}]$ ; (iv) $[y + {1\over 3}, -x + y+{2\over 3}, -z + {2\over 3}]$ ; (v) $[-x + y+{2\over 3}, x - {1\over 3}, -z + {2\over 3}]$ ; (vi) $[-x + {2\over 3}, -y + {1\over 3}, -z + {1\over 3}]$ ; (vii) $[-y - {1\over 3}, -x + y+{1\over 3}, -z + {1\over 3}]$ ; (viii) $[x-y - {1\over 3}, x - {2\over 3}, -z + {1\over 3}]$ .

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 71| Part 5| September 2015| Pages 555-561

doi:10.1107/S2052520615015838

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