Integrated geochemical, geoelectrical, and UAV-based methods for analyzing the Gzeylülaı landslide Çnkae(aakl, Tükyeri)

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dc.authorid0000-0003-2024-0565
dc.authorid0000-0002-3112-5258
dc.contributor.authorErenoglu, Oya
dc.contributor.authorUlugergerli, Emin
dc.contributor.authorErenoglu, R. Cueneyt
dc.contributor.authorAkbas, Abdullah
dc.contributor.authorErginal, A. Evren
dc.date.accessioned2026-02-03T12:03:22Z
dc.date.available2026-02-03T12:03:22Z
dc.date.issued2025
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe number of reactivations increased in the G & uuml;zelyal & imath;-Erenk & ouml;y landslide area after 2013 in & Ccedil;anakkale, T & uuml;rkiye, where historical landslide activity has been recorded since 1875. This area is home to numerous summer residences and experiences ongoing slow-moving landslide activity along a 400-m-long slope, extending from the heavily trafficked & Ccedil;anakkale-& Idot;zmir highway to the coastline. In this study, the nature of the reactivations was evaluated by considering the conditioning and triggering factors that contributed to the landslide. The evaluation was based on geochemical analyses, field observations, geoelectric measurements, and unmanned aerial vehicle (UAV) data. The results revealed that the sliding occurred along a moist slip surface, rich in various clay minerals such as illite, montmorillonite, and vermiculite, at a depth of approximately 4.5 m, as determined by ERT (Electrical Resistivity Tomography). Vertical movements within the landslide area, including rises and subsidences, accounted for changes of up to 0.1 m between 2013 and 2023. Chemical Index of Weathering (CIW), Chemical Index of Alteration (CIA), and Plagioclase Index of Alteration (PIA) calculations obtained from the X-ray fluorescence (XRF) spectroscopy analysis indicate that the sliding surface is subjected to strong weathering, and these values are compatible with the X-Ray diffraction (XRD) data.
dc.description.sponsorshipScientific Research Coordination Unit of Canakkale Onsekiz Mart University [SBA-2021-3628]
dc.description.sponsorshipThis work was supported by the Scientific Research Coordination Unit of Canakkale Onsekiz Mart University, project number: SBA-2021-3628. We thank M. & Idot;zmirli (Canakkale Special Provincial Administration) for assisting us in gathering ERT data.
dc.identifier.doi10.55730/1300-0985.1974
dc.identifier.issn1300-0985
dc.identifier.issue4
dc.identifier.scopus2-s2.0-105007342820
dc.identifier.scopusqualityQ2
dc.identifier.trdizinid1333784
dc.identifier.urihttps://doi.org/10.55730/1300-0985.1974
dc.identifier.urihttps://search.trdizin.gov.tr/tr/yayin/detay/1333784
dc.identifier.urihttps://hdl.handle.net/20.500.12428/35057
dc.identifier.volume34
dc.identifier.wosWOS:001500660000005
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakTR-Dizin
dc.language.isoen
dc.publisherTubitak Scientific & Technological Research Council Turkey
dc.relation.ispartofTurkish Journal of Earth Sciences
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WOS_20260130
dc.subjectG & uuml;zelyal & imath
dc.subjectlandslide
dc.subjectUAV monitoring
dc.subjectgeoelectrical slip detection
dc.subjectlandslide reactivation
dc.subjectdoi
dc.titleIntegrated geochemical, geoelectrical, and UAV-based methods for analyzing the Gzeylülaı landslide Çnkae(aakl, Tükyeri)
dc.typeArticle

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