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Fig. 3 | Swiss Journal of Geosciences

Fig. 3

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

Fig. 3

Example of field criteria used to establish relative deformation chronologies and separate fracture data into kinematically homogeneous subsets. a Cross-cutting relationship between two fracture sets within an outcrop of Upper Malm limestone (Plattenkalk Fm.; outcrop 51, see Fig. 1; Table 1 for location). A normal fault plane is cross-cut and slightly offset by vertical strike-slip faults and therefore regarded as being relatively older. b Illustration of the separation of the fracture dataset into two kinematically homogeneous subsets. Fracture data are illustrated as lower hemisphere equal area projections

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