Investigation of the nature of slip surface using geochemical analyses and 2-D electrical resistivity tomography: a case study from Lapseki area, NW Turkey

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dc.authoridEkinci, Yunus Levent/0000-0003-4966-1208
dc.authoridDemirci, Alper/0000-0002-8710-6232
dc.contributor.authorErginal, Ahmet Evren
dc.contributor.authorOzturk, Beyhan
dc.contributor.authorEkinci, Yunus Levent
dc.contributor.authorDemirci, Alper
dc.date.accessioned2025-01-27T20:57:57Z
dc.date.available2025-01-27T20:57:57Z
dc.date.issued2009
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe nature and subsurface structure of the slip surface of a landslide was studied on the basis of geochemical analyses and 2-D electrical resistivity tomography (ERT) survey. Head scarp and lateral slip surfaces of the landslide marked by clear slickensided shear planes were composed of the average amounts of clayey silt (32.5%) and sand (67.5%). Energy dispersive X-ray spectroscopy (EDX) data revealed the enrichment of Si (23.24%), Fe (12.2%), Al (9.51%) and C (8.34%) in the elemental composition of the disturbed slip surface. From X-ray diffractometry (XRD) data, six main clay types were determined, such as Volkonskoite, Halloysite, Ferrosilite, Saponite, Illite and Nontronite. The ERT survey displayed that the landslide developed as a reactivation on the upper part of an old landslide body.
dc.description.sponsorshipOnsekiz Mart University Research Foundation [2008/32]
dc.description.sponsorshipWe thank Ercan Bilir and Muhammed Zeynel Ozturk for fieldwork assistance and Ali Sungur for his effort in grainsize analyses. Drs. Emin U. Ulugergerli and Su r ha O r zden are thanked for their useful suggestions. We also thank Dr. Tolga Bekler for his permission to use the resistivity meter in this research. This study was carried out thanks to the financial support provided by C, anakkale Onsekiz Mart University Research Foundation (Project number: 2008/32). Journal reviewers are thanked for their valuable comments that greatly improved the paper.
dc.identifier.doi10.1007/s00254-008-1594-4
dc.identifier.endpage1175
dc.identifier.issn0943-0105
dc.identifier.issue6
dc.identifier.scopus2-s2.0-70349865288
dc.identifier.scopusqualityN/A
dc.identifier.startpage1167
dc.identifier.urihttps://doi.org/10.1007/s00254-008-1594-4
dc.identifier.urihttps://hdl.handle.net/20.500.12428/26565
dc.identifier.volume58
dc.identifier.wosWOS:000269076800003
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer
dc.relation.ispartofEnvironmental Geology
dc.relation.publicationcategoryinfo:eu-repo/semantics/openAccess
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectLandslide
dc.subjectSlip surface material
dc.subjectGeochemical analysis
dc.subjectERT
dc.subjectRotational slide
dc.subjectLapseki
dc.titleInvestigation of the nature of slip surface using geochemical analyses and 2-D electrical resistivity tomography: a case study from Lapseki area, NW Turkey
dc.typeArticle

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