Fig. 5From: Multiple detachments during thin-skinned deformation of the Swiss Central Jura: a kinematic model across the ChasseralCompiled stratigraphy of the Mesozoic cover. Thicknesses of units above the Argovien sequence are estimated for the Combe Grède area (Schori 2014), whereas thicknesses of older units are based on unsmoothed depth grids of Engler and Sommaruga (2013) at CH1903/LV03 576035 211909. h u , h 1–5 height of important horizons above the basal décollement (h0)Back to article page