Towards The Mitigation Of The Tsunami Risk By Submarine Mass Failures In The Gulf Of Corinth: The Xylocastro Resort Town Case Study

Author:

Charalampakis M.,Stefatos A.,Ferentinos G.,Mpourdopoulos K.

Publisher

Springer Netherlands

Reference25 articles.

1. Ambraseys, N.N., 1962. Data for the investigation of the seismic seawaves in the eastern Mediterranean. Bull. Seismol. Soc. Am. 52: 895–913.

2. Antonopoulos, J., 1980. Data from investigation on seismic sea-waves events in the eastern Mediterranean from birth of Christ to 1980 AD (6 parts). Annal. Geofis. 33: 141–248.

3. Charalampakis, M., Stefatos, A., Hasiotis, T. & Ferentinos, G., 2005. Morphology, structure and evolution of the Xylocastro basin bounding fault margin, central Gulf of Corinth. International Symposium on the Geodynamics of Eastern Mediterranean: Active Tectonics of the Aegean Region, 15-18 June 2005, Istanbul, Turkey.

4. Galanopoulos, A.G., 1960. Tsunamis observed on the coasts of Greece from antiquity to present time. Ann. Geofis. 13: 369–386.

5. Ferentinos, G., Papatheodorou, G. & Collins, M.B., 1988. Sediment transport processes on an active submarine fault escarpment: Gulf of Corinth, Greece. Marine Geology 83: 43–61.

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