Fig. 9From: Multiple detachments during thin-skinned deformation of the Swiss Central Jura: a kinematic model across the ChasseralForward modelled cross-section of the Chasseral area. Some branch bisector trajectories, that acted as flow deflector lines used by the fault-parallel flow method, are illustrated with dot-dashed lines. Note that the short wavelength folds at the northern Chasseral mountainside are not modelled in detailBack to article page