Charge ordered structure of magnetite Fe(3)O(4) below the Verwey transition
The crystal structure of highly stoichiometric magnetite (Fe3O4) below the Verwey transition has been refined from high-resolution neutron and synchrotron x-ray powder-diffraction data. The refined model has a monoclinic P2/c symmetry cell with orthorhombic Pmca pseudosymmetry constraints on the ato...
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Fformat: | Journal article |
Iaith: | English |
Cyhoeddwyd: |
2002
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