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Swiss Journal of Geosciences
Fig. 10 | Swiss Journal of Geosciences

Fig. 10

From: Tectonic evolution around the Mont Terri rock laboratory, northwestern Swiss Jura: constraints from kinematic forward modelling

Fig. 10Fig. 10

Forward-modelled cross section of the Mont Terri and Mont Russelin using the classical scenario with a basal detachment. The syncline that is above regional between Mont Terri and Clos du Doubs anticlines relies on a local high formed by a basement horst. The initial Clos du Doubs anticline is formed by a thrust wedge (like in the Clos du Doubs section, see Fig. 9), but is enhanced by a series of NNE-trending steep thrusts. Section trace is shown in Figs. 2 and 4 and stratigraphic legend from Figs. 2 and 3

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