title: Magnetite: Preferred Orientation on the Basal Plane of Partially Reduced Hematite.
abstract: Crystallites of two different orientations have been observed in the polycrystalline magnetite layer formed by carbon monoxide reduction on the basal plane of a hematite single crystal. The relative reducibility of hematite and magnetite ores may be related to this double orientation.
authors.forename: R O
authors.initials: RO
authors.lastname: Keeling
authors.forename: D A
authors.initials: DA
authors.lastname: Wick