Fig.Ā 9From: Tectonic evolution around the Mont Terri rock laboratory, northwestern Swiss Jura: constraints from kinematic forward modellingForward-modelled cross section of the Clos du Doubs to constrain and validate the thrust sequence of the forward models for the Mont TerriāMont Russelin section (Fig.Ā 10). Section trace is shown in Figs.Ā 1, 2, and 4. Initial basement-related extensional faults are offset by an out-of-sequence series of thrust-wedges that connected the basal detachment to the detachment in the overlying Staffelegg Formation to form a tectonic wedge and a presently surfacing back-thrust. The final-stage geometry shown under (4) was not modelled in detail to fit with the present-day geometry. The stratigraphic units are described in Figs.Ā 2 and 3 Back to article page