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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Príomhchruthaitheoirí: Wright, J, Attfield, J, Radaelli, P
Formáid: Journal article
Teanga:English
Foilsithe / Cruthaithe: 2002