The coordination of Co2+ions in Co substituted magnetites, Fe3−xCoxO4, with x⩽0.04
Author:
Publisher
Elsevier BV
Subject
General Physics and Astronomy
Reference6 articles.
1. 57Fe Hyperfine Fields in Magnetite (Fe3O4)
2. Recoilless-Fraction Ratios forFe57in Octahedral and Tetrahedral Sites of a Spinel and a Garnet
3. The B-site Mössbauer linewidth in Fe3O4
4. Magnetic properties of the garnets Bi0·8Ca2χT2·2-2.χFe5-χVχ]O12
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