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dc.contributor.authorUtkucu, Murat
dc.contributor.authorBudakoğlu, Emrah
dc.contributor.authorYalçin, Hilal
dc.contributor.authorDurmuş, Hatice
dc.date.accessioned2021-12-15T10:45:27Z
dc.date.available2021-12-15T10:45:27Z
dc.date.issued2014
dc.identifier.issn1301-2894
dc.identifier.urihttps://app.trdizin.gov.tr/makale/TVRZeU5UQTVPUT09/23-ekim-2011-van-dogu-anadolu-depremi-nin-mw-7-1-sismotektonik-ozellikleri
dc.identifier.urihttp://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/2898
dc.description.abstract23 Ekim 2011 Van depreminin geniş bant uzak-alan cisim dalga şekillerinin sonlu-fay modellemesi deprem kırılmasının ters faylanma olduğunu ve tek taraflı olarak GB’ya yayıldığını göstermiştir. Kırılma 5 km altında kısıtlı kalmış, yaklaşık 5.5 m en büyük
dc.description.abstractThe finite-fault modelling of the 23 October 2011 Van earthquake using teleseismic broadband body waveforms has shown that the earthquake occured as a result of reverse faulting and its rupture propogated unilaterally toward SW. The rupture confined to
dc.language.isoTurkish
dc.sourceYerbilimleri
dc.title23 Ekim 2011 Van (Doğu Anadolu) Depremi’Nin (Mw=7.1) Sismotektonik Özellikleri
dc.identifier.issue2
dc.identifier.startpage87
dc.identifier.endpage108
dc.identifier.volume35


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