Tectonic development of western Anatolian extensional province

dc.authoridYILMAZ, YÜCEL/0000-0003-2340-027X
dc.authoridGurer, Omer Feyzi/0000-0001-7210-769X
dc.authorwosidYILMAZ, YÜCEL/GVU-7421-2022
dc.authorwosidGurer, Omer Feyzi/A-9893-2008
dc.contributor.authorYilmaz, Yucel
dc.contributor.authorGurer, Omer Feyzi
dc.date.accessioned2023-10-19T15:12:49Z
dc.date.available2023-10-19T15:12:49Z
dc.date.issued2023
dc.department-temp[Yilmaz, Yucel] Kadir Has Univ, Istanbul, Turkiye; [Gurer, Omer Feyzi] Kocaeli Univ, Jeoloji Muhendisligi Bolumu, Muhendisl Fak, Kocaeli, Turkiyeen_US
dc.description.abstractWestern 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.citation3
dc.identifier.doi10.1080/00206814.2023.2209865en_US
dc.identifier.issn0020-6814
dc.identifier.issn1938-2839
dc.identifier.scopus2-s2.0-85159275253en_US
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.1080/00206814.2023.2209865
dc.identifier.urihttps://hdl.handle.net/20.500.12469/5542
dc.identifier.wosWOS:000987118000001en_US
dc.identifier.wosqualityQ1
dc.khas20231019-WoSen_US
dc.language.isoenen_US
dc.publisherTaylor & Francis Incen_US
dc.relation.ispartofInternational Geology Reviewen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectMetamorphic Core ComplexEn_Us
dc.subjectBuyuk-Menderes GrabenEn_Us
dc.subjectBalikesir Transfer ZoneEn_Us
dc.subjectStrain-Rate FieldEn_Us
dc.subjectEpisodic 2-Stage ExtensionEn_Us
dc.subjectM-W=6.3 Lesvos EarthquakeEn_Us
dc.subjectHellenic Subduction ZoneEn_Us
dc.subjectStrike-Slip DeformationEn_Us
dc.subjectSw-Trending SelendiEn_Us
dc.subjectGediz GrabenEn_Us
dc.subjectMetamorphic Core Complex
dc.subjectBuyuk-Menderes Graben
dc.subjectBalikesir Transfer Zone
dc.subjectStrain-Rate Field
dc.subjectEpisodic 2-Stage Extension
dc.subjectM-W=6.3 Lesvos Earthquake
dc.subjectHellenic Subduction Zone
dc.subjectWestern Anatoliaen_US
dc.subjectStrike-Slip Deformation
dc.subjectCrustal extensionen_US
dc.subjectSw-Trending Selendi
dc.subjectGraben developmenten_US
dc.subjectGediz Graben
dc.subjectNeogeneen_US
dc.titleTectonic development of western Anatolian extensional provinceen_US
dc.typeArticleen_US
dspace.entity.typePublication

Files

Original bundle

Now showing 1 - 1 of 1
No Thumbnail Available
Name:
5542.pdf
Size:
3.79 MB
Format:
Adobe Portable Document Format
Description:
Tam Metin / Full Text