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Swiss Journal of Geosciences
Fig. 3 | Swiss Journal of Geosciences

Fig. 3

From: Investigating distant effects of the Moesian promontory: brittle tectonics along the western boundary of the Getic unit (East Serbia)

Fig. 3

Aa: Asymmetric grains (b type of Doblas et al. 1997); Ab: calcite growth, diameter of coin is 2.2 cm; Ba: lunate fracture with trailing gouge material (Petit 1987); Bb: trail material; Bc: curving grooves, compass for scale; C: crosscutting systems of „carrot-shaped” gauge markings (Doblas et al. 1997), hammer tip for scale; D; displacement of calcite-filled tension gashes along shear joints, pencil for scale; E: gouging-grain grooves (Doblas, 1998) with asperity ploughing (Means 1987), two generations of tension gashes are also visible, pencil for scale; F crystallization on the lee side of asperities (Petit 1987), pencil for scale; G: four asymmetric elevations (Doblas 1998) with tension gashes? Pencil for scale; H: spall marks and plucking markings (Doblas et al. 1997), coin for scale, arrow indicates slip sense

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