Fig. 4From: Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?Seismic section (a) and its interpretation (b) of a section cross-cutting the Kalat syncline in the east. See Fig. 2 for approximate location. North-verging rooting down to the basement cuts the section up to Upper Cretaceous strata. A lower splay of the thrust branches into the Lower Cretaceous that acts as a layer parallel detachmentBack to article page