Fig. 4From: Investigating distant effects of the Moesian promontory: brittle tectonics along the western boundary of the Getic unit (East Serbia)Geological map of the Miocene–Pliocene sedimentary basin east of the town of Despotovac (location given on Fig. 2). Observation points are marked as black dots. Observed faults with striations (arrows indicate slip sense), as well as calculated tensors are provided in stereoplots (red circle: maximum compression; white rectangle: intermediate axis; blue triangle: extensional axis)Back to article page