Fig. 5From: Investigating distant effects of the Moesian promontory: brittle tectonics along the western boundary of the Getic unit (East Serbia)Photographs indicating the interpretation of field evidences of fault activity in the area of the Miocene–Pliocene sedimentary basin east of the town of Despotovac (map on Fig. 4). a, b Synsedimentary normal fault in Middle Miocene sediments. c, d Normal faulting in Middle Miocene sediments. e, f Fault plane of a sinistral strike slip fault in Pliocene sedimentsBack to article page