Fig. 5From: Characterising the CI and CI-like carbonaceous chondrites using thermogravimetric analysis and infrared spectroscopy3 μm/11 μm versus H2O (wt. %) determined from TGA (a) and phyllosilicate abundances (vol. %) (b) from King et al. (2015). The similarity in H2O abundance, 3 μm/11 μm ratio and phyllosilicate abundance suggests that Ivuna and Orgueil experienced equal degrees of aqueous alteration. Relative to Y-82162, Y-980115 contains a higher abundance of H2O and phyllosilicate and has an increased 3 μm/11 μm ratio, suggesting that it experienced less dehydrationBack to article page