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dc.contributor.authorTan, O.
dc.contributor.authorPabucu, Z.
dc.contributor.authorTaprdamaz, M.C.
dc.contributor.authorNan, S.
dc.contributor.authorErgintav, S.
dc.contributor.authorEyidoǧan, H.
dc.contributor.authorAksoy, E.
dc.contributor.authorKuluöztürk, F.
dc.date.accessioned2021-12-16T10:13:12Z
dc.date.available2021-12-16T10:13:12Z
dc.date.issued2011
dc.identifier.issn948276
dc.identifier.urihttps://doi.org/10.1029/2011GL047702
dc.identifier.urihttp://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/13455
dc.description.abstractA destructive earthquake (Mw = 6.1) occurred on the northeast end of the Palu segment of the East Anatolian Fault System (EAFS, eastern Turkey) on 8 March 2010. The spatial distribution of aftershocks suggests that the Palu segment does not terminate to t
dc.language.isoEnglish
dc.publisherBlackwell Publishing Ltd
dc.sourceGeophysical Research Letters
dc.titleAftershock study and seismotectonic implications of the 8 March 2010 Kovanclar (Elazǧ, Turkey) earthquake (MW = 6.1)
dc.typeArticle
dc.identifier.issue11
dc.identifier.doi10.1029/2011GL047702
dc.identifier.scopus2-s2.0-79958850417
dc.identifier.volume38


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