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dc.contributor.authorYilmaz I.
dc.contributor.authorÜstünkaya M.
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T09:12:49Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T09:12:49Z
dc.date.issued2004
dc.identifier.issn1435-9529
dc.identifier.urihttps://dx.doi.org/10.1007/s10064-004-0229-6
dc.identifier.urihttps://hdl.handle.net/20.500.12418/4500
dc.description.abstractThe consolidation properties of clay samples from a marine environment were examined. Index, triaxial and odeometer tests were performed on the undisturbed/disturbed clay samples from 13 boreholes in the Gemlik Gulf (Bursa-Turkey). Laboratory tests indicated that the clays are soft and have a high moisture content and hence are highly compressible. The majority of the clays are unconsolidated due to the accretion rate being faster than the dissipation of pore water. © Springer-Verlag 2004.en_US
dc.language.isoengen_US
dc.relation.isversionof10.1007/s10064-004-0229-6en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectClay soilen_US
dc.subjectConsolidationen_US
dc.subjectMarineen_US
dc.subjectSaturated conditionen_US
dc.subjectShear strengthen_US
dc.titleUnconsolidated clays from the inner shore of the Gemlik Gulf in the Marmara Sea (Bursa-Turkey)en_US
dc.typearticleen_US
dc.relation.journalBulletin of Engineering Geology and the Environmenten_US
dc.contributor.departmentYilmaz, I., Department of Geology, Faculty of Enginering, Cumhuriyet University, Sivas 58140, Turkey -- Üstünkaya, M., Best Ltd., Ostim, Ankara, Turkeyen_US
dc.identifier.volume63en_US
dc.identifier.issue2en_US
dc.identifier.endpage139en_US
dc.identifier.startpage133en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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