Cl. Hayward et al., POLARIZED SINGLE-CRYSTAL RAMAN-SPECTROSCOPY OF SINHALITE, MGALBO(4), Spectrochimica acta. Part A: Molecular spectroscopy, 50(7), 1994, pp. 1287-1294
Polarised single-crystal Raman spectra for sinhalite have been collect
ed at 80 K over the range 1300-10 cm-1. All 36 of the first-order Rama
n bands predicted by the factor group analysis (FGA) of the olivine st
ructure type have been observed and assigned. Sinhalite has the smalle
st unit cell volume of any crystal with the olivine structure and is s
ignificantly more distorted than are the silicate olivines. This leads
to distortion-related consequences in the vibrational spectra, such a
s greater wavenumber ranges for each type of mode and reduced Raman in
tensity for symmetric BO4 modes. Intense Raman bands in the region 796
-468 cm-1 are assigned to BO4 rotations/translations which deform the
Al-O bond without displacement of the aluminium atoms which lie on the
M1 sites. Raman-active modes involving Ml cation displacements are in
compatible with the FGA.