Bulletin of the Geological Society of Greece Vol. 40, 2007 TECTONO-SEDIMENTARY EVOLUTION AND RATES OF TECTONIC UPLIFT OF THE SFAKIA COASTAL ZONE, SOUTHWESTERN CRETE Skourtsos E. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment Pope R. Geographical Sciences, University of Derby Triantaphyllou M. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment https://doi.org/10.12681/bgsg.16649 Copyright © 2018 E. Skourtsos, R. Pope, M. V. Triantaphyllou To cite this article: Skourtsos, E., Pope, R., & Triantaphyllou, M. (2007). TECTONO-SEDIMENTARY EVOLUTION AND RATES OF TECTONIC UPLIFT OF THE SFAKIA COASTAL ZONE, SOUTHWESTERN CRETE. Bulletin of the Geological Society of Greece, 40(1), 475-487. doi:https://doi.org/10.12681/bgsg.16649 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 21/02/2020 00:42:18 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, May, Πρακτικά 11ου Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 2007 TECTONO-SEDIMENTARY EVOLUTION AND RATES OF TECTONIC UPLIFT OF THE SFAKIA COASTAL ZONE, SOUTHWESTERN CRETE Skourtsos E.1, Pope R.2, and Triantaphyllou M. V.1 National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Panepistimioupolis Zografou, 154 21,
[email protected],
[email protected] Geographical Sciences, University of Derby, Derby, DE22 1GB, UK,
[email protected] Abstract Sfakia lies within a narrow coastal zone at the southwestern foothills of the Lefka Ori Mt. Here a segment of the South Cretan margin is preserved onshore, a struc ture that represents a neotectonic structure with continuous activity since the Upper Miocene.