Fig. 11From: Multiple detachments during thin-skinned deformation of the Swiss Central Jura: a kinematic model across the ChasseralArea-height diagram for the kinematically viable cross-section (Figs. 8, 9). The black graph is constructed by using uplifted reference horizons in the Vallon de St-Imier, whereas the grey graph is based on correct reference horizons. The deviation between the two graphs illustrates the error due to the use of uplifted reference horizons. EA excess area, D total displacement, d displacement on the upper detachment, h u height of upper detachment, Cr top Cretaceous, Po top Portlandian, Se top Séquanien, Do top Dogger, Ke top Keuper sequenceBack to article page