Uplift of the western Anatolia and its relationship with crustal deformation

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dc.authorid0000-0003-1248-9811en_US
dc.authorid-en_US
dc.authorscopusid6506140632en_US
dc.authorscopusid-en_US
dc.authorwosid-en_US
dc.authorwosid-en_US
dc.contributor.authorKomut, Tolga
dc.contributor.authorPürçek, İlker
dc.date.accessioned2023-05-29T05:35:00Z
dc.date.available2023-05-29T05:35:00Z
dc.date.issued2021en_US
dc.departmentFakülteler, Mühendislik Fakültesi, Jeofizik Mühendisliği Bölümü
dc.description.abstractA peneplain plateau, as a primary evidence for a recently elevated topography, represents the top surface of the western Anatolian crust that is deforming under an extensional regime. Vertical (up-flow) support of the hot mantle beneath the western Anatolia is responsible for the elevation of the crust. Residual topography anomaly models which indicate uplift of the crust and hence dynamic support of the mantle to the crust were calculated using useful sets of crustal thickness data. A distinct anomaly of a new residual topography model based on receiver functions in Anatolia marks an exhumed metamorphic core complex in the region. Mantle flow beneath the west Anatolian region is probably responsible for extensive exhumation of the metamorphic core complex and distributed extension in N–S direction. GPS velocities’ smooth differentiation indicates uniform diffusivity. Residual topography anomaly, which is one of the important pieces of evidence of the uplift, can also be compared with velocities related to diffuse N–S crustal extension in the region. Various pieces of evidence suggest strong relationships between the mantle dynamics, increased elevation, and extension of the crust in western Anatolia.en_US
dc.identifier.citationKomut, T., & Pürçek, İ. (2021). Uplift of the western anatolia and its relationship with crustal deformation. Arabian Journal of Geosciences, 14(17) doi:10.1007/s12517-021-08088-xen_US
dc.identifier.doi10.1007/s12517-021-08088-x
dc.identifier.issn1866-7511
dc.identifier.issue17en_US
dc.identifier.scopus2-s2.0-85112315383
dc.identifier.urihttps://doi.org/10.1007/s12517-021-08088-x
dc.identifier.urihttps://hdl.handle.net/20.500.12428/4218
dc.identifier.volume14en_US
dc.indekslendigikaynakScopus
dc.institutionauthorKomut, Tolga
dc.institutionauthorPürçek, İlker
dc.language.isoen
dc.publisherSpringer Science and Business Media Deutschland GmbHen_US
dc.relation.ispartofArabian Journal of Geosciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectDistributed crustal extensionen_US
dc.subjectMantle flowen_US
dc.subjectResidual topographyen_US
dc.subjectWestern Anatoliaen_US
dc.titleUplift of the western Anatolia and its relationship with crustal deformation
dc.typeArticle

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