Fig. 9From: Alpine peak pressure and tectono-metamorphic history of the Monte Rosa nappe: evidence from the cirque du Véraz, upper Ayas valley, ItalySchematic E–W lithological section from the Monte Rosa metagranite intrusive suite, Monte Rosa basement complex, and finally the over-thrusted Zermatt-Saas nappe. Structural position of whiteschist analyzed in Luisier et al. (2019) and the whiteschist of this study are indicatedBack to article page