Fig. 5From: Structure, geometry and kinematics of the northern Adula nappe (Central Alps)Outcrop-scale structures in the Zapport Valley area. a Internal Mesozoic layer constituted by a narrow syncline (729900/151900) b Internal Mesozoic layer folded by FZ (727500/151250) c Interference pattern produced by superimposed folding between FU and FZ and interpretative schema (725950/151470). d Leis phase fold (727680/151150)Back to article page