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Evaluation of active faulting and earthquake secondary effects in Lefkada Island, Ionian Sea, Greece: An overview

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dc.contributor.author Rondoyanni, T en
dc.contributor.author Sakellariou, M en
dc.contributor.author Baskoutas, J en
dc.contributor.author Christodoulou, N en
dc.date.accessioned 2014-03-01T02:08:53Z
dc.date.available 2014-03-01T02:08:53Z
dc.date.issued 2012 en
dc.identifier.issn 0921030X en
dc.identifier.uri http://hdl.handle.net/123456789/29747
dc.subject Active faulting en
dc.subject Athani fault en
dc.subject Earthquake hazard en
dc.subject Lefkada earthquake en
dc.subject Neotectonic mapping en
dc.subject.other active fault en
dc.subject.other aftershock en
dc.subject.other deformation en
dc.subject.other earthquake en
dc.subject.other faulting en
dc.subject.other seismic hazard en
dc.subject.other seismotectonics en
dc.subject.other strike-slip fault en
dc.subject.other Aegean Islands en
dc.subject.other Greece en
dc.subject.other Ionian Islands en
dc.subject.other Lefkada en
dc.title Evaluation of active faulting and earthquake secondary effects in Lefkada Island, Ionian Sea, Greece: An overview en
heal.type journalArticle en
heal.identifier.primary 10.1007/s11069-011-0080-6 en
heal.identifier.secondary http://dx.doi.org/10.1007/s11069-011-0080-6 en
heal.publicationDate 2012 en
heal.abstract Based on neotectonic mapping, analysis of active deformation through tectonic data and the Coulomb stress changes caused by major earthquakes, the active faults in Lefkada Island were evaluated. Descriptions of historic and recent earthquakes were also taken into consideration as well as the seismotectonic data concerning the last strong seismic event of 2003. According to detailed field observations, among the active and neotectonic faults that have been identified, regarding seismic hazard, the most important can be considered the Athani fault. It is running parallel to and near the west coast and shows marked similarity with the northern branch of the offshore transform fault of Kefalonia-Lefkada. These two dextral strike-slip faults exhibit same structure and state of stress as well. Moreover, the Coulomb stress changes associated with the 2003 earthquake, well correlated with the spatial aftershock pattern, are positive in the area of the Athani fault. Attention has been also focused on the geologic hazard in relation to earthquake associated phenomena, such as surface rupturing, landslides and rockfalls, liquefaction and tsunamis. The fact that surface deformation is repeated in an identical way during past and recent earthquakes provides a great advantage for the seismic protection of the island. © 2012 Springer Science+Business Media B.V. en
heal.journalName Natural Hazards en
dc.identifier.doi 10.1007/s11069-011-0080-6 en
dc.identifier.volume 61 en
dc.identifier.issue 2 en
dc.identifier.spage 843 en
dc.identifier.epage 860 en


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