Tectonic Development of Western Anatolian Extensional Province

dc.authorid YILMAZ, YÜCEL/0000-0003-2340-027X
dc.authorid Gurer, Omer Feyzi/0000-0001-7210-769X
dc.authorwosid YILMAZ, YÜCEL/GVU-7421-2022
dc.authorwosid Gurer, Omer Feyzi/A-9893-2008
dc.contributor.author Yilmaz, Yucel
dc.contributor.author Gurer, Omer Feyzi
dc.date.accessioned 2023-10-19T15:12:49Z
dc.date.available 2023-10-19T15:12:49Z
dc.date.issued 2023
dc.department-temp [Yilmaz, Yucel] Kadir Has Univ, Istanbul, Turkiye; [Gurer, Omer Feyzi] Kocaeli Univ, Jeoloji Muhendisligi Bolumu, Muhendisl Fak, Kocaeli, Turkiye en_US
dc.description.abstract Western Anatolia is one of the fastest-extending continental regions. The approximately N-S extension, in three phases, generated grabens of various ages and trends. The first phase occurred during the late Oligocene-Early Miocene and caused the exhumation of the high-grade metamorphic rocks in the footwall of the low-angle detachment fault(s). This phase caused the NNE trending grabens, particularly in the northern areas. The second phase happened in the Late Miocene. The initial rise of the central horst (the Bozdag Horst) bounded by the detachment faults corresponds to this extension. The third phase generated the dominant morphotectonic entities of western Anatolia, the E-W trending normal faults, and the associated grabens in Quaternary. Western Anatolia began rotating counter-clockwise since the westerly escape of the Anatolian Plate reached the region and caused the generation of the NE-NW trending conjugated strike-slip faults and the consequent grabens along the coastal areas in the Holocene. en_US
dc.identifier.citationcount 3
dc.identifier.doi 10.1080/00206814.2023.2209865 en_US
dc.identifier.issn 0020-6814
dc.identifier.issn 1938-2839
dc.identifier.scopus 2-s2.0-85159275253 en_US
dc.identifier.scopusquality Q1
dc.identifier.uri https://doi.org/10.1080/00206814.2023.2209865
dc.identifier.uri https://hdl.handle.net/20.500.12469/5542
dc.identifier.wos WOS:000987118000001 en_US
dc.identifier.wosquality Q1
dc.khas 20231019-WoS en_US
dc.language.iso en en_US
dc.publisher Taylor & Francis Inc en_US
dc.relation.ispartof International Geology Review en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.scopus.citedbyCount 6
dc.subject Metamorphic Core Complex En_Us
dc.subject Buyuk-Menderes Graben En_Us
dc.subject Balikesir Transfer Zone En_Us
dc.subject Strain-Rate Field En_Us
dc.subject Episodic 2-Stage Extension En_Us
dc.subject M-W=6.3 Lesvos Earthquake En_Us
dc.subject Hellenic Subduction Zone En_Us
dc.subject Strike-Slip Deformation En_Us
dc.subject Sw-Trending Selendi En_Us
dc.subject Gediz Graben En_Us
dc.subject Metamorphic Core Complex
dc.subject Buyuk-Menderes Graben
dc.subject Balikesir Transfer Zone
dc.subject Strain-Rate Field
dc.subject Episodic 2-Stage Extension
dc.subject M-W=6.3 Lesvos Earthquake
dc.subject Hellenic Subduction Zone
dc.subject Western Anatolia en_US
dc.subject Strike-Slip Deformation
dc.subject Crustal extension en_US
dc.subject Sw-Trending Selendi
dc.subject Graben development en_US
dc.subject Gediz Graben
dc.subject Neogene en_US
dc.title Tectonic Development of Western Anatolian Extensional Province en_US
dc.type Article en_US
dc.wos.citedbyCount 9
dspace.entity.type Publication

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