(A) Schematic drawing showing the three main trends of the D₂ planar surface arranged in a sinistral S₂-C₂-C’₂ like anastomosed transpressional system. This representative outcrop comes from the Bans valley, southeastern Inner Pelvoux. (B) Picture 7B shows the steeply dipping S₂ cleavage observed within the Peyre-Arguet mafic granulite, retrogressed into amphibolite. Very thin seams of leucosome are located parallel to the compositional layering, and S₂ or C₂ foliation. (C) Picture 7C shows a strongly layered stromatic migmatite that has been reworked by solid-state deformation during sinistral shearing along a C’₂ plane.