The crystal structure of a new metastable tellurium (IV) oxyfluoride Te3O5F2 [non-centrosymmetric P21 space group] is unusually complex with 15 different Te polyhedra. It is built of giant cylindrical columns of oxide units connected via weak Te-F bonds. A strict O/F order is evidenced and a structural comparison with Sb3O2F5 shows that these two phases derive, by a different mechanism, from the anion-excess fluorite superstructure type. Surprisingly, in these two structures is observed a full gradation of various polyhedra of tellurium (IV) or antimony (III) with the oxygen atom ensuring a strong framework at the centre of these structures (cylinders for Te phase and layers for Sb one), and more and more F anions moved away at the periphery of these strong units, connecting these units via weak Te-F or Sb-F bonds. This well illustrates the different roles played by oxygen and fluorine atoms in the oxyfluorides of cations presenting an electronic lone pair E (5s2 in the case of Te4+ cation), in relation with the non-linear properties of these phases.
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