An X-ray absorption study on O 1s edge was carried out on natural oxides with rutile-type crystal structure – the minerals rutile (TiO2), pyrolusite (MnO2), cassiterite (SnO2) and plattnerite (β-PbO2). Despite the chemical bonding being essentially ionic, the differences in the outer electron shell of cations clearly influence post-edge features of XAS spectra. The implications of site symmetry on coordination environment are emphasized for [MO6] octahedra (with quite regular geometry in cassiterite) and for the isosceles triangle [OM3] that displays either two long plus one shorter (pyrolusite and plattnerite) or two short plus one longer (rutile and cassiterite) M–O distances, with M–O–M bond angles always close to 100° plus twice 130°.Theoretical modelling of XAS spectra was carried out. Details of O 1s absorption spectra like the presence of a single post-edge feature for plattnerite and cassiterite may be interpreted by the separation or mixing between O 2p and M nd plus mixing with M ns and np states. Spectra features are commented in relation to crystal structure details but the energy shift assigned for the O K-edge in cassiterite still lacks a plausible explanation.
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