Extensional crustal-scale shear zones in the Western Cyclades (Kea, Greece)
2006
Müller, Monika | Grasemann, Bernhard | Edwards, Michael A. | Draganits, Erich | Voit, Klaus | Iglseder, Christoph | Zámolyi, András | Petrakakis, Konstantin | Philipp, Sonja | Leiss, Bernd | Vollbrecht, Axel | Tanner, David | Gudmundsson, Agust
Intense seismicity and intensely developed active and ancient fault systems are common to the Aegean Region. Extending/ thinning crust involves a complex interplay of (1) Gulf of Corinth riftexpansion, (2) west- and south-ward retreat of the Hellenic Trench, (3) westward impingement of the Anatolian Platen, and/or (4) propagation of the Anatolian Fault system into the Aegean. New geological/structural investigations on Kea (also known as Tzia), in the Western Cyclades reveal a low angle crustal-scale, detachment-type ductile shear zone probably formed during Miocene extension and thinning of the continental crust...
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Эту запись предоставил Georg-August-Universität Göttingen