“…These IR bands were assigned to symmetric
stretching vibrations of [
] silicate units containing tetrahedral units with zero to four non-bridging oxygens, namely, tectosilicate, disilicate, metasilicate, pyrosilicate, and orthosilicate units denoted as Q4, Q3, Q2, Q1, and Q0 respectively [26] . The IR features allow distinguishing bands located at about cm −1 , cm −1 , cm −1 , near 900 cm −1 , near 850 cm −1 of each dominant at the tectosilicate, disilicate, metasilicate, pyrosilicate, and orthosilicate units [27] .…”