Quaternary rock uplift rates and their implications for the western flank of the North Anatolian Fault restraining bend; inferences from fluvial terrace ages

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dc.authorid0000-0002-9571-7914
dc.authorid0000-0001-5253-028X
dc.authorid0000-0002-6755-8426
dc.authorid0000-0001-5886-0773
dc.authorid0000-0001-8254-8974
dc.authorid0000-0002-7485-6157
dc.authorid0000-0001-8598-8596
dc.contributor.authorMcClain, Kevin P.en_US
dc.contributor.authorYıldırım, Cengizen_US
dc.contributor.authorCiner, Attilaen_US
dc.contributor.authorŞahin, Sefaen_US
dc.contributor.authorSarıkaya, Mehmet Akifen_US
dc.contributor.authorÖzcan, Orkanen_US
dc.contributor.authorGüneç Kıyak, Nafiyeen_US
dc.contributor.authorÖztürk, Tuğbaen_US
dc.date.accessioned2020-11-30T11:18:08Z
dc.date.available2020-11-30T11:18:08Z
dc.date.issued2020-10-01
dc.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümüen_US
dc.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.description.abstractIn the western flank of the North Anatolian Fault restraining bend (i.e., Central Pontides), the Filyos River incises through the uplifting Karabük Range, creating the ~1.7-km-deep Filyos River Gorge on the hanging wall of the reverse Karabük Fault. Seven fluvial strath terrace levels are preserved in this gorge. optically stimulated luminescence ages from quartz-rich sediments of five terrace levels reveal an average long-term rock uplift rate of 0.45 ± 0.02 mm yr?1 with an unsteady pattern of uplift during the last 542 ± 24 kyr. Uplift rates of 1.52 ± 0.6 and 0.74 ± 0.3 mm yr?1 occurred before 366 ± 19 kyr, followed by lower rates of ~0.1 and 0.31 mm yr?1 through present. These later uplift rates may reflect relatively slower tectonic rates since ~366 kyr, with closer similarity to regional uplift rates of ~0.3 mm yr?1 yielded from the eastern flank of the Central Pontides. The Karabük Range fluvial terraces are near the North Anatolian Fault, meaning pre- ~366 kyr uplift rates may be a glimpse of the highest Central Pontides Quaternary rock uplift rates on uplifting hanging wall blocks activated by the restraining bend. When we consider offshore seismic reflection data, the focal mechanism solution of the Bartın Earthquake, onshore structural data, and regional tectonic geomorphology, the western flank of the Central Anatolian Plateau's northern margin is propagating northward as a growing orogenic wedge with a positive flower-structure geometry.en_US
dc.description.versionPublisher's Versionen_US
dc.identifier.citationMcClain, Kevin P., Yıldırım, C., Ciner, A., Şahin, S., Mehmet Akif, S., Özcan, O., Güneç Kıyak, N. & Öztürk, T. (2020). Quaternary rock uplift rates and their implications for the western flank of the North Anatolian Fault restraining bend; inferences from fluvial terrace ages. Tectonics, 39(10), 1-22. doi:10.1029/2019TC005993en_US
dc.identifier.doi10.1029/2019TC005993
dc.identifier.endpage22
dc.identifier.issn0278-7407
dc.identifier.issn1944-9194
dc.identifier.issue10
dc.identifier.scopus2-s2.0-85094132086
dc.identifier.scopusqualityQ1
dc.identifier.startpage1
dc.identifier.urihttps://hdl.handle.net/11729/2977
dc.identifier.urihttp://dx.doi.org/10.1029/2019TC005993
dc.identifier.volume39
dc.identifier.wosWOS:000598731000008
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.indekslendigikaynakScience Citation Index Expanded (SCI-EXPANDED)en_US
dc.institutionauthorÖztürk, Tuğbaen_US
dc.institutionauthorid0000-0001-8598-8596
dc.language.isoenen_US
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.publisherBlackwell Publishing Ltden_US
dc.relation.ispartofTectonicsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectNorth Anatolian Faulten_US
dc.subjectMarmara Seaen_US
dc.subjectFault zoneen_US
dc.subjectCentral pontidesen_US
dc.subjectFluvial terraceen_US
dc.subjectOSLen_US
dc.subjectRestraining benden_US
dc.subjectRock upliften_US
dc.subjectTurkeyen_US
dc.subjectEarthquakesen_US
dc.subjectLuminescenceen_US
dc.subjectOffshore oil well productionen_US
dc.subjectFlower structuresen_US
dc.subjectOptically stimulated luminescenceen_US
dc.subjectRegional tectonicsen_US
dc.subjectRock uplift ratesen_US
dc.subjectSeismic reflection dataen_US
dc.subjectFaultingen_US
dc.subjectEarthquakeen_US
dc.subjectFocal mechanismen_US
dc.subjectGeomorphologyen_US
dc.subjectHanging wallen_US
dc.subjectLuminescence datingen_US
dc.subjectOrogenyen_US
dc.subjectQuaternaryen_US
dc.subjectReverse faulten_US
dc.subjectTerraceen_US
dc.subjectUpliften_US
dc.subjectBartinen_US
dc.subjectKarabuken_US
dc.subjectPontidesen_US
dc.subjectYenice Riveren_US
dc.titleQuaternary rock uplift rates and their implications for the western flank of the North Anatolian Fault restraining bend; inferences from fluvial terrace agesen_US
dc.typeArticleen_US
dspace.entity.typePublication

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