Fig. 15From: Fossil oceanic core complexes in the Alps. New field, geochemical and isotopic constraints from the Tethyan Aiguilles Rouges Ophiolite (Val d’Hérens, Western Alps, Switzerland)Schematic model of the oceanic lithosphere from the Piemonte-Liguria basin based on observations from the Aiguilles Rouges Ophiolite. The model shows 3 snapshots on the interplay between deformation and magmatism. For further discussion, see textBack to article page