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Fig. 5 | Swiss Journal of Geosciences

Fig. 5

From: Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?

Fig. 5

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 strata

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