Fig. 5From: 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 cutting parallel to the main Kalat syncline strike. See Fig. 2 for approximate location. Several basement-related normal faults appear in pre-Jurassic rocks. ESE-verging thrust rooting down into a basement normal fault. Minor offsets occur in Upper Cretaceous strataBack to article page