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Fig. 15). La vibration de libration des OH à 664 cm -1 , que l'on retrouve dans les deux spectres, est associée à la kérolite. Cette vibration se déplace à 655 cm -1 dans le cas de la saponite mais on ne distingue pas un tel déplacement dans les spectres de l'aquarium 4, Chapitre I 1023 cm -1 sont associées aux vibrations Si-O de la kérolite, 1974. ,
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, une bande à 795 cm -1 et deux bandes situées à 856 et 886 cm -1 correspondant au mode de flexion hors-plan du groupe carbonate (?2CO3) (Farmer, 1974) (Fig. 15), correspondant à la vibration Mg-O (à ne pas confondre avec celles des Mg-O octaédriques des silicates de magnésium à 530-540 cm -1 ), vol.3515, pp.3658-3659
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