Fig. 11From: Three-dimensional modelling of folds, thrusts, and strike-slip faults in the area of Val de Ruz (Jura Mountains, Switzerland)“Tectonic” thickness of Muschelkalk, measured in a vertical direction from the top of the Muschelkalk down to the top of the basement, and shown in an oblique view. This thickness includes layer repetition by thrusting, leading to high thickness in anticlines. Red compass needle indicates northBack to article page