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dc.contributor.authorTeze, Okan
dc.contributor.authorOzcep, Ferhat
dc.contributor.authorKarabulut, Savas
dc.contributor.authorImre, Nazire
dc.date.accessioned2021-03-02T23:08:37Z
dc.date.available2021-03-02T23:08:37Z
dc.date.issued2012
dc.identifier.citationKarabulut S., Teze O., Ozcep F., Imre N., "A geophysical study on soil conditions in flood-affected Selimpasa area, Istanbul, Turkey", CURRENT SCIENCE, cilt.102, sa.2, ss.320-326, 2012
dc.identifier.issn0011-3891
dc.identifier.othervv_1032021
dc.identifier.otherav_10b34727-8ffe-4231-9411-3ded42c4530d
dc.identifier.urihttp://hdl.handle.net/20.500.12627/16723
dc.description.abstractMulti-channel analysis of surface waves (MASVV) and micrometer array measurements (MAM) have been carried out in the flood-prone areas of Selimpasa, Kavakli, Ortakoy and Kadikoy in Turkey to understand several soil problems, especially soil amplification during earthquakes. In the region, there are now more than 80 geotechnical boreholes with SPT and laboratory test data, as also MASW-MAM geophysical measurements at more than 100 locations. All these data have been evaluated to classify the soils according to Eurocode 8, determine soil amplification and finally to obtain a microzonation map. According to the Eurocode soil classification system, there are D, B and C type soils in the area of study. In the final microzonation map, the study area is divided into three sub-regions based on shear wave (Vs) velocities sub-region A (Vs velocities higher than 420 m/s), sub-region B (Vs velocities between 360 and 420 m/s) and sub-region C (Vs velocities lower than 360 m/s). Results show that there are clear relationships between Vs 30 and flood damage effect. Vs 30: 180 m/s is characteristic of zone with D type soil, which is transported alluvial soil. Vs 30 < 180 zones define the limits of the areas affected by floods in the study region.
dc.language.isoeng
dc.subjectDoğa Bilimleri Genel
dc.subjectTemel Bilimler
dc.subjectÇOK DİSİPLİNLİ BİLİMLER
dc.subjectTemel Bilimler (SCI)
dc.titleA geophysical study on soil conditions in flood-affected Selimpasa area, Istanbul, Turkey
dc.typeMakale
dc.relation.journalCURRENT SCIENCE
dc.contributor.departmentEmek Geophys & Geotechn Co , ,
dc.identifier.volume102
dc.identifier.issue2
dc.identifier.startpage320
dc.identifier.endpage326
dc.contributor.firstauthorID202899


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