The study of the kinematics of the Late Cretaceous to Early Eocene sediments of the Ulukışla Basin in Central southern Turkey has identified a major extensional structure that has in part exhumed high-pressure metamorphic rocks: the Ivriz Detachment. Check it out here!
Documenting one of the surface expressions of large scale extension that affected the central and southern Anatolian region – the Ivriz Detachment