In order to assign the bands in the IR spectra of silicates to the app
ropriate normal vibrations, a vibrational model has been proposed, A c
omplex silicooxygen ring is considered as a 'unit cell' composed of th
e appropriate number of [SiO4](4-) tetrahedra. According to this model
, in the ring silicates spectra we have to observe bands due to intern
al vibrations of individual tetrahedra and bands corresponding exclusi
vely to the ring structure. Change in the tetrahedra symmetry from Td
(ideal tetrahedron) to C-2v (tetrahedron in a ring) and then to the ri
ng symmetry: D-3h, D-4h and D-6h (ideal rings) with respect to reducib
le representations makes it possible to differentiate between the band
s due to ring structure (pseudo-lattice vibrations) and internal modes
of tetrahedra. It has been established that in the case of all ideal
rings there is only one IR active vibrational mode, namely the one sym
metric with respect to the axis of the highest fold, i.e. A(2)'' in th
e case of 3-membered rings and A(2u) in the case of 4- and 6-membered
rings. The model proposed has been verified for different membered rin
g silicates. (C) 1998 Elsevier Science B.V.