Testing miocene remagnetization of bey Dağları: Timing and amount of neogene rotations in SW Turkey

The current model for this orocline involves a 25−30° counterclockwise (CCW) rotation of the Bey Dağları region, which exposes upper Cretaceous to Eocene platform carbonates and lower Miocene flysch deposits. In this model the rotation has to postdate a Miocene remagnetization, which would not exclude non-synchroneity between rotations of the western and eastern limbs of the Aegean orocline.