Fig. 9From: Investigating distant effects of the Moesian promontory: brittle tectonics along the western boundary of the Getic unit (East Serbia)Schematic sketch of oroclinal bending and clockwise rotation of the Dacia mega-unit around the Moesian promontory, and activation of dextral strike-slip faults (Cerna-Jiu and Timok), as well as the expected direction of extension during this process (white double arrows). The research area is indicated by red rectangleBack to article page