Fig. 14
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Thermobarometric modelling of metapelitic sample MCE338 located in the Cortical Pelvoux. (A) Chemical profile of a garnet. (B) T-XH2O diagram calculated with a pressure of 0.5 GPa, the mineral assemblage of the sample indicates a H2O content of 1.47 wt%. (C) Pseudosection calculated in the MnNCKFMASH system. Modelling of the Qcmp factor of the mineral composition of (D) biotite based on MgO, FeO, MnO, Al2O3 and SiO2 contents, (E) muscovite based on Na2O, K2O, CaO, Al2O3, FeO, MgO and SiO2 contents, and (F) plagioclase based on K2O, Na2O, CaO, Al2O3 and SiO2 contents (Tab. S2). Bi: Biotite; Mu: muscovite; Crd: Cordierite; Kfs: K-feldspar; Pl: Plagioclase; Gt: Garnet; and: Andalousite; ky: Kyanite; sill: Sillimanite; Opx: Orthopyroxene; q: Quartz; melt: silicate liquid.
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