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Swiss Journal of Geosciences
Fig. 2 | Swiss Journal of Geosciences

Fig. 2

From: Multiple detachments during thin-skinned deformation of the Swiss Central Jura: a kinematic model across the Chasseral

Fig. 2

Overview of the Chasseral area. Geological units are modified from the swisstopo GeoCover (Swisstopo 2012) and the Geological Atlas 1:25000 (Schär et al. 1971) and overlie a hillshade model (Swisstopo 2011) that illustrates the topography of the terrain. Dip data is taken from Swisstopo (2012). The oldest exposed geological units belong to the upper Dogger sequence. Traces of faults and thrusts are from Schori (2014). The lower hemisphere equal-area projection shows bedding poles and fold axes for the northern Chasseral mountainside at the Combe Grède (Schori 2014)

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