@incollection{gledocs_11858_00-1735-0000-0001-3479-9,
author = {Müller, Monika and Grasemann, Bernhard and Edwards, Michael A. and Draganits, Erich and Voit, Klaus and Iglseder, Christoph and Zámolyi, András and Petrakakis, Konstantin},
editor = {Philipp, Sonja and Leiss, Bernd and Vollbrecht, Axel and Tanner, David and Gudmundsson, Agust},
title = {Extensional crustal-scale shear zones in the Western Cyclades (Kea, Greece)},
booktitle = {11. Symposium "Tektonik, Struktur- und Kristallingeologie"},
year = {2006-03},
publisher = {Universitätsverlag Göttingen},

abstract = {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...},
note = { \url {http://hdl.handle.net/11858/00-1735-0000-0001-3479-9}},
}