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Raman and infrared spectra of calcurmolite were recorded and interpreted from the uranium and molybdenum polyhedra, water molecules and hydroxyls point of view. UO bond lengths in uranyl and MoO bond lengths in MoO 6 octahedra were calculated and OH…O bond lengths were inferred from the spectra. The mineral calcurmolite is characterised by bands assigned to the vibrations of the UO 2 units. These units provide intense Raman bands at 930, 900 and 868 and 823 cm −1 . These bands are attributed to the anti‐symmetric and symmetric stretching modes of the UO 2 units, respectively. Raman bands at 794, 700, 644, 378 and 354 cm −1 are attributed to vibrations of the MoO 4 units. The bands at 693 and 668 cm −1 are assigned to the anti‐symmetric and symmetric A g modes of the terminal MO 2 units. Similar bands are observed at 797 and 773 cm −1 for koechlinite and 798 and 775 cm −1 for lindgrenite. It is probable that some of the bands in the low wavenumber region are attributable to the bending modes of MO 2 units.
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Frost et al. (2008) studied this question.
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