“…The in situ method can be applied to single crystals and to grains within thin sections. This method is based on linear relationships between the CO 2 content in wt% and the Raman intensity ratio of the CO 2 -stretching mode against two Si-O streching modes of the cordierite structure in a certain orientation (Kolesov & Geiger, 2000;Kaindl et al, 2006). The incorporation and orientation of CO 2 molecules in the structural channels of cordierite were investigated using various methods including DTA and dehydration studies (Sugiura, 1959), X-ray and neutron diffraction (e.g., Cohen et al, 1977;Armbruster, 1985), IR spectroscopy (Farrell & Newnham, 1967;Goldman et al, 1977;Le Breton, 1989;Vry et al, 1990;Kalt, 2000), proton NMR spectroscopy (Carson et al, 1982), quasi-elastic neutron scattering (Winkler et al, 1994b), and quantum mechanical calculations (Winkler et al, 1994a).…”