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Displacement field and fault model for the September 7, 1999 Athens earthquake inferred from ERS2 satellite radar interferometry

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dc.contributor.author Kontoes, C en
dc.contributor.author Elias, P en
dc.contributor.author Sykioti, O en
dc.contributor.author Briole, P en
dc.contributor.author Remy, D en
dc.contributor.author Sachpazi, M en
dc.contributor.author Veis, G en
dc.contributor.author Kotsis, I en
dc.date.accessioned 2014-03-01T01:15:33Z
dc.date.available 2014-03-01T01:15:33Z
dc.date.issued 2000 en
dc.identifier.issn 0094-8276 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/13583
dc.subject Fault Model en
dc.subject Radar Interferometry en
dc.subject.classification Geosciences, Multidisciplinary en
dc.title Displacement field and fault model for the September 7, 1999 Athens earthquake inferred from ERS2 satellite radar interferometry en
heal.type journalArticle en
heal.identifier.primary 10.1029/2000GL008510 en
heal.identifier.secondary http://dx.doi.org/10.1029/2000GL008510 en
heal.language English en
heal.publicationDate 2000 en
heal.abstract On September 7, 1999, a moderate (M-n = 5.9) normal faulting earthquake occurred in the northwest of Athens (Hellas) causing heavy damages and casualties. Using interferometric combinations of ERS2 SAR images, we analyzed the coseismic deformation field. Two fringes are observed south of the Fill mountain, up to the coastline of the Elefsis gulf. They correspond to 56 mm increase in slant range. Modeling the earthquake as a dislocation in an elastic half-space, we inverted the interferometric data to assess the fault location and geometry and the amplitude of the coseismic slip. The model suggests similar to 300 mm slip on an 18 km long blind fault composed of two pieces. The intersection of the fault plane with the Earth surface is located in the Fill mountain with a similar to N120 degrees orientation. en
heal.publisher AMER GEOPHYSICAL UNION en
heal.journalName GEOPHYSICAL RESEARCH LETTERS en
dc.identifier.doi 10.1029/2000GL008510 en
dc.identifier.isi ISI:000166311700007 en
dc.identifier.volume 27 en
dc.identifier.issue 24 en
dc.identifier.spage 3989 en
dc.identifier.epage 3992 en


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