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Fig. 5 | Swiss Journal of Geosciences

Fig. 5

From: Tectonics of the Neuchâtel Jura Mountains: insights from mapping and forward modelling

Fig. 5

Initial shallow interpretation of the structures based on field measurements, existing geological maps (Fallot et al. 1968; Pasquier and Burkhard 2013), structural data from Sommaruga (1997), DEM analysis, shallow well data (Pasquier et al. 2013) and geophysical studies (Pasquier 2008; Pasquier and Turberg 2009). Seimic reflector horizons from Sommaruga (1997) were converted to depth with a new velocity model. Discrepancies between the section and the seismic line result from the lateral offset of the seismic line and the cross-section trace (the line was shot 1.5 km east of the section in the Vallée de La Brévine and 1 km west of the section near Travers). This near-surface cross-section was the base on which the forward model was built. The position of the cross section is shown in Fig. 4

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