Fig. 6From: Along-strike shear-sense reversal in the Vals-Scaradra Shear Zone at the front of the Adula Nappe (Central Alps, Switzerland)Overprinting relations in a piece of chlorite-bearing mica schist with quartz veins (Adula-Nappe basement, R: 720,151, H: 156,109). Duplicated layer in the hinge of Zapport-phase fold suggest the existence of pre-Zapport isoclinal folds (Sorreda Phase)Back to article page