Fig. 9 

Part 1 of the 2D kinematic forward model from the Geneva Basin to the Bienne Valley (deformation steps 0 to 5). In the individual deformation steps, the active thrust is shown in black and inactive thrusts are coloured in red. The numbering of the faults corresponds to the sequence of deformation. Step 0 corresponds to the Northern Alpine Foreland stage prior to the Jura thrusting and represents the initial layer cake model supplemented by the information about the basement depth (Fig. 8). Step 1 indicates the first deformation and step 11, the last one. The Mesozoic cover shown in the forward model, has been built on the Near-Top Basement line (Fig. 8). The 1st and 2nd deformation steps the folding of the Crêt de la Neige Anticline related to the movement along the Reculet Thrust. The steps 3 to 5 show the movement along the Crêt Chalam Thrust with its imbrication, leading to the Bellecombe Anticline. The algorithm used in Move^tm version 2020.1 with the resulting shortening is detailed for each step