Fig. 2From: Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?Geological map with most important structural features and stratigraphic description of the Kalat syncline. Locations of sample sites P01–P07 are indicated as red stars. Approximate location of seismic profiles of Figs. 3, 4 and 5 and the map of Fig. 15 are shown as black outlinesBack to article page