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dc.contributor.authorBerndt, Christopheren_US
dc.contributor.authorYıldırım, Cengizen_US
dc.contributor.authorÇiner, Tahsin Attilaen_US
dc.contributor.authorStrecker, Manfred R.en_US
dc.contributor.authorErtunç, Gülgünen_US
dc.contributor.authorSarıkaya, Mehmet Akifen_US
dc.contributor.authorÖzcan, Orkanen_US
dc.contributor.authorÖztürk, Tuğbaen_US
dc.contributor.authorKıyak Güneç, Nafiyeen_US
dc.date.accessioned2019-01-02T03:23:22Z
dc.date.available2019-01-02T03:23:22Z
dc.date.issued2018-12-01
dc.identifier.citationBerndt, C., Yıldırım, C., Çiner, A., Strecker, M. R., Ertunç, G., Sarıkaya, M. A., Özcan, O., Öztürk, T., Kiyak, N. G. (2018). Quaternary uplift of the northern margin of the central anatolian plateau: New OSL dates of fluvial and delta-terrace deposits of the kızılırmak river, black sea coast, turkey. Quaternary Science Reviews, 201, 446-469.en_US
dc.identifier.issn0277-3791
dc.identifier.otherWOS:000452934700027
dc.identifier.urihttps://hdl.handle.net/11729/1436
dc.identifier.urihttp://dx.doi.org/10.1016/j.quascirev.2018.10.029
dc.description.abstractWe analysed the interplay between coastal uplift, sea level change in the Black Sea, and incision of the Kizilirmak River in northern Turkey. These processes have created multiple co-genetic fluvial and marine terrace sequences that serve as excellent strain markers to assess the ongoing evolution of the Pontide orogenic wedge and the growth of the northern margin of the Central Anatolian Plateau. We used high-resolution topographic data, OSL ages, and published information on past sea levels to analyse the spatiotemporal evolution of these terraces; we derived a regional uplift model for the northward advancing orogenic wedge that supports the notion of laterally variable uplift rates along the flanks of the Pontides. The best-fit uplift model defines a constant long-term uplift rate of 0.28 +/- 0.07 m/ka for the last 545 ka. This model explains the evolution of the terrace sequence in light of active tectonic processes and superposed cycles of climate-controlled sea-level change. Our new data reveal regional uplift characteristics that are comparable to the inner sectors of the Central Pontides; accordingly, the rate of uplift diminishes with increasing distance from the main strand of the restraining bend of the North Anatolian Fault Zone (NAFZ). This spatial relationship between the regional impact of the restraining bend of the NAFZ and uplift of the Pontide wedge thus suggests a strong link between the activity of the NAFZ, deformation and uplift in the Pontide orogenic wedge, and the sustained lateral growth of the Central Anatolian Plateau flank.en_US
dc.language.isoengen_US
dc.publisherPergamon-Elsevier Science Ltden_US
dc.relation.isversionof10.1016/j.quascirev.2018.10.029
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.sourceQuaternary Science Reviewsen_US
dc.subjectQuaternaryen_US
dc.subjectOSL datingen_US
dc.subjectBlack Seaen_US
dc.subjectPontidesen_US
dc.subjectNorth Anatolian Fault Zoneen_US
dc.subjectOrogenic wedgeen_US
dc.subjectKizilirmak Riveren_US
dc.subjectMISen_US
dc.subjectTurkeyen_US
dc.subjectCentral andean plateauen_US
dc.subjectSouthern marginen_US
dc.subjectPuna plateauen_US
dc.subjectDose-ratesen_US
dc.subjectCosmic-rayen_US
dc.subjectClimateen_US
dc.subjectGrowthen_US
dc.subjectEvolutionen_US
dc.subjectLuminescenceen_US
dc.subjectIncisionen_US
dc.subjectClimate changeen_US
dc.subjectClimate modelsen_US
dc.subjectManagement information systemsen_US
dc.subjectRiversen_US
dc.subjectTectonicsen_US
dc.subjectSea levelen_US
dc.subjectContinental marginen_US
dc.subjectCrustal deformationen_US
dc.subjectDating methoden_US
dc.subjectDeltaic depositen_US
dc.subjectFluvial depositen_US
dc.subjectMarine isotope stageen_US
dc.subjectNorth Anatolian Faulten_US
dc.subjectOrogenic belten_US
dc.subjectSea level changeen_US
dc.subjectSpatial analysisen_US
dc.subjectTectonic wedgeen_US
dc.subjectTerraceen_US
dc.subjectUpliften_US
dc.subjectBlack Sea Coast [Turkey]en_US
dc.titleQuaternary uplift of the northern margin of the Central Anatolian Plateau: New OSL dates of fluvial and delta-terrace deposits of the Kizilirmak River, Black Sea coast, Turkeyen_US
dc.typearticleen_US
dc.description.versionPublisher's Versionen_US
dc.contributor.departmentIşık Üniversitesi, Fen-Edebiyat Fakültesi, Fizik Bölümüen_US
dc.contributor.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.contributor.authorID182420
dc.contributor.authorID169366
dc.contributor.authorID19592
dc.contributor.authorID148686
dc.contributor.authorID103106
dc.identifier.volume201
dc.identifier.startpage446
dc.identifier.endpage469
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.relation.publicationcategoryBelirsizen_US
dc.contributor.institutionauthorÖztürk, Tuğba


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