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Swiss Journal of Geosciences
Fig. 7 | Swiss Journal of Geosciences

Fig. 7

From: Outcrop-scale fracture systems in the Alpine foreland of central northern Switzerland: kinematics and tectonic context

Fig. 7

Fracture kinematics across the study area: a relationship between slip lineation and fracture dip angle for all faults and mode-II fractures discussed. The vast majority of fractures show strike-slip kinematics but dip-slip (reverse and normal faulting) is also common. b Distribution of strike-slip, reverse and normal slip indicators according to tectonic units. FJ Folded Jura, DTJ Deformed Tabular, TJ Tabular Jura (compare Figs. 1, 6). N number of measurements

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