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Fig. 5 | Swiss Journal of Geosciences

Fig. 5

From: Three-dimensional modelling of folds, thrusts, and strike-slip faults in the area of Val de Ruz (Jura Mountains, Switzerland)

Fig. 5

Line balancing for the input profiles in Fig. 4. The bars show the length of the top of the respective stratigraphic units, e.g. “Malm” means the length of the top of the Malm. Numbers on the horizontal axis are meters. Average percentage of shortening of the layers is indicated for each profile. All profiles are well balanced, i.e. differences in bed length are small

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