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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Hlavní autoři: Wright, J, Attfield, J, Radaelli, P
Médium: Journal article
Jazyk:English
Vydáno: 2002