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dc.contributor.authorZarif, Halil
dc.contributor.authorOzcep, Ferhat
dc.contributor.authorKorkmaz, Burcu
dc.contributor.authorKarabulut, Savas
dc.date.accessioned2021-03-04T18:59:25Z
dc.date.available2021-03-04T18:59:25Z
dc.date.issued2011
dc.identifier.citationKarabulut S., Ozcep F., Korkmaz B., Zarif H., "Urban Seismic Microzonation Studies at Small Scales: Sisli/Istanbul (Turkey)", ARABIAN JOURNAL FOR SCIENCE AND ENGINEERING, cilt.36, ss.75-87, 2011
dc.identifier.issn2193-567X
dc.identifier.othervv_1032021
dc.identifier.otherav_8d8ca073-5acc-4c25-8499-ce4e8eabd83b
dc.identifier.urihttp://hdl.handle.net/20.500.12627/95682
dc.identifier.urihttps://doi.org/10.1007/s13369-010-0012-x
dc.description.abstractThe main purpose of this study is to provide a high-resolution application of urban seismic microzonation. A probabilistic seismic hazard analysis was undertaken in the study area using Poisson probabilistic approaches. The resulting hazard is characterized by a 15% probability that a given level of acceleration will be exceeded in a 50-year period. Using deterministic seismic hazard analysis, the magnitudes were estimated by a quadruple rupture model (with three different fault lengths, 108, 119 and 174km) of the North Anatolian Fault Zone in the Marmara Region. Using both analyses (deterministic and probabilistic), the magnitude of the design earthquake was taken as 7.6. From this design earthquake, accelerations were estimated for several distances (from 25 to 50 km) using several attenuation relationships. In the second phase of the study, soil amplification factors and site characteristic periods were determined and estimated by seismic measurements and Standard Penetration Test data for the Sisli area of central Istanbul. Microtremor and earthquake data were evaluated to compare the characteristic site period data obtained. According to Eurocode soil classifications, the study area mainly consists of B type soils. A small part of the study area has C and A type soils. Characteristic site periods obtained by seismic methods agree with strong (earthquake) and weak (ambient noise) motion spectral values in some parts of the study area. Finally, a seismic microzonation map was prepared for integrated use, incorporating all geophysical and geotechnical data.
dc.language.isoeng
dc.subjectÇOK DİSİPLİNLİ BİLİMLER
dc.subjectDoğa Bilimleri Genel
dc.subjectTemel Bilimler (SCI)
dc.subjectTemel Bilimler
dc.titleUrban Seismic Microzonation Studies at Small Scales: Sisli/Istanbul (Turkey)
dc.typeMakale
dc.relation.journalARABIAN JOURNAL FOR SCIENCE AND ENGINEERING
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume36
dc.identifier.issue1
dc.identifier.startpage75
dc.identifier.endpage87
dc.contributor.firstauthorID59989


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