“…However, this calcite presents There is probably some overlapping between calcite and Ca-oxalate bands, for example on the double peak at 874 and 780 cm −1 . The peak at 1,730 cm −1 can be related to carbonyl stretching (Cappitelli et al 2007). The quartz bands (1,200, 1,150, 1,030, 799, 512, and 469 cm −1 ) are all in good agreement with quartz absorbances displayed by other authors (e.g., Etchepare et al 1974;Williams 1995. The XRD and FTIR spectra evidenced certain specific characteristics and associations between the neoformed mineral phases.…”