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Probabilistic Seismic Hazard Assessment for Lake Van Basin, Turkey

dc.authorid Selcuk, Levent/0000-0002-7060-8260
dc.authorscopusid 16246356400
dc.authorscopusid 35746828200
dc.authorscopusid 12753032900
dc.authorwosid Beyaz, Turgay/Aac-4103-2020
dc.authorwosid Selçuk, Azad/Iwu-3071-2023
dc.contributor.author Selcuk, Levent
dc.contributor.author Selcuk, Azad Saglam
dc.contributor.author Beyaz, Turgay
dc.date.accessioned 2025-05-10T16:49:27Z
dc.date.available 2025-05-10T16:49:27Z
dc.date.issued 2010
dc.department T.C. Van Yüzüncü Yıl Üniversitesi en_US
dc.department-temp [Selcuk, Levent; Selcuk, Azad Saglam] Yuzuncu Yil Univ, Dept Geol Engn, Architectural Engn Fac, TR-65080 Van, Turkey; [Beyaz, Turgay] Pamukkale Univ, Dept Geol Engn, Sch Engn, TR-20017 Kinikli, Denizli, Turkey en_US
dc.description Selcuk, Levent/0000-0002-7060-8260 en_US
dc.description.abstract The seismic hazard for the Lake Van basin is computed using a probabilistic approach, along with the earthquake data from 1907 to present. The spatial distribution of seismic events between the longitudes of 41-45A degrees and the latitudes of 37.5-40A degrees, which encompasses the region, indicates distinct seismic zones. The positions of these zones are well aligned with the known tectonic features such as the Tutak-CaldA +/- ran fault zone, the A-zalp fault zone, the GevaAY fault zone, the Bitlis fault zone and KarlA +/- ova junction where the North Anatolian fault zone and East Anatolian fault zone meet. These faults are known to have generated major earthquakes which strongly affected cities and towns such as Van, MuAY, Bitlis, A-zalp, Muradiye, CaldA +/- ran, ErciAY, Adilcevaz, Ahlat, Tatvan, GevaAY and GurpA +/- nar. The recurrence intervals of M (s) a parts per thousand yen 4 earthquakes were evaluated in order to obtain the parameters of the Gutenberg-Richter measurements for seismic zones. More importantly, iso-acceleration maps of the basin were produced with a grid interval of 0.05 degrees. These maps are developed for 100- and 475- year return periods, utilizing the domestic attenuation relationships. A computer program called Sistehan II was utilized to generate these maps. en_US
dc.description.woscitationindex Science Citation Index Expanded
dc.identifier.doi 10.1007/s11069-010-9517-6
dc.identifier.endpage 965 en_US
dc.identifier.issn 0921-030X
dc.identifier.issue 3 en_US
dc.identifier.scopus 2-s2.0-77956109660
dc.identifier.scopusquality Q1
dc.identifier.startpage 949 en_US
dc.identifier.uri https://doi.org/10.1007/s11069-010-9517-6
dc.identifier.uri https://hdl.handle.net/20.500.14720/1839
dc.identifier.volume 54 en_US
dc.identifier.wos WOS:000281324200020
dc.identifier.wosquality Q2
dc.language.iso en en_US
dc.publisher Springer en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.subject Lake Van Basin en_US
dc.subject Peak Ground Acceleration en_US
dc.subject Probabilistic Approach en_US
dc.subject Return Period en_US
dc.title Probabilistic Seismic Hazard Assessment for Lake Van Basin, Turkey en_US
dc.type Article en_US

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