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dc.contributor.authorYıldırım, Cengiztr_TR
dc.contributor.authorMelnick, Danielen_US
dc.contributor.authorBallato, Paoloen_US
dc.contributor.authorSchildgen, Taylor F.en_US
dc.contributor.authorEchtler, Helmut P.en_US
dc.contributor.authorErginal, Ahmet Evrentr_TR
dc.contributor.authorKıyak, Nafiye Güneçtr_TR
dc.contributor.authorStrecker, Manfreden_US
dc.date.accessioned2015-01-15T23:02:15Z
dc.date.available2015-01-15T23:02:15Z
dc.date.issued2013-12
dc.identifier.citationYildirim, C., Melnick, D., Ballato, P., Schildgen, T., Echtler, H., Erginal, A., . . . Strecker, M. (2013). Differential uplift along the northern margin of the central anatolian plateau: Inferences from marine terraces. QUATERNARY SCIENCE REVIEWS, 81, 12-28. doi:10.1016/j.quascirev.2013.09.011en_US
dc.identifier.issn0277-3791
dc.identifier.issn1873-457X
dc.identifier.otherWOS:000328443400002
dc.identifier.urihttp://hdl.handle.net/11729/472
dc.identifier.urihttp://dx.doi.org/10.1016/j.quascirev.2013.09.011
dc.description.abstractEmerged marine terraces and paleoshorelines along plate margins are prominent geomorphic markers that can be used to quantify the rates and patterns of crustal deformation. The northern margin of the Central Anatolian Plateau has been interpreted as an actively deforming orogenic wedge between the North Anatolian Fault and the Black Sea. Here we use uplifted marine terraces across principal faults on the Sinop Peninsula at the central northern side of the Pontide orogenic wedge to unravel patterns of Quaternary faulting and orogenic wedge behavior. We leveled the present-day elevations of paleoshorelines and dated marine terrace deposits using optically stimulated luminescence (OSL) to determine coastal uplift. The elevations of the paleoshorelines vary between 4 +/- 0.2 and 67 +/- 1.4 m above sea level and OSL ages suggest terrace formation episodes during interglacial periods at ca 125, 190, 400 and 570 ka, corresponding to marine isotopic stages (MIS) 5e, 7a, 11 and 15. Mean apparent vertical displacement rates (without eustatic correction) deduced from these terraces range between 0.02 and 0.18 mm/a, with intermittent faster rates of up to 0.26 mm/a. We obtained higher rates at the eastern and southern parts of the peninsula, toward the hinterland, indicating non-uniform uplift across the different morphotectonic segments of the peninsula. Our data are consistent with active on- and offshore faulting across the Sinop Peninsula. When integrated with regional tectonic observations, the faulting pattern reflects shortening distributed over a broad region of the northern margin of the Central Anatolian Plateau during the Quaternaryen_US
dc.language.isoenen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTDen_US
dc.relation.isversionof10.1016/j.quascirev.2013.09.011
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.sourceQuaternary Science Reviewsen_US
dc.subjectOrogenic Plateausen_US
dc.subjectCentral Anatolian Plateauen_US
dc.subjectPlateau marginsen_US
dc.subjectCentral Pontidesen_US
dc.subjectOrogenic wedgesen_US
dc.subjectBlack Seaen_US
dc.subjectMarine terracesen_US
dc.subjectUplift rateen_US
dc.titleDifferential uplift along the northern margin of the Central Anatolian Plateau: inferences from marine terracesen_US
dc.typearticleen_US
dc.description.versionPublisher's Versionen_US
dc.contributor.departmentIsik University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.contributor.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümütr_TR
dc.contributor.authorIDTR182420
dc.contributor.authorIDTR20371
dc.contributor.authorIDTR41807
dc.identifier.volume81
dc.identifier.startpage12
dc.identifier.endpage28
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US


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