Collision-related granite magma genesis, potential sources and tectono-magmatic evolution: comparison between central, northwestern and western Anatolia (Turkey)

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dc.authoridIlbeyli, Nurdane/0000-0002-0557-8771
dc.contributor.authorIlbeyli, Nurdane
dc.contributor.authorKibici, Yasar
dc.date.accessioned2024-09-18T20:06:22Z
dc.date.available2024-09-18T20:06:22Z
dc.date.issued2009
dc.departmentHatay Mustafa Kemal Üniversitesien_US
dc.description.abstractThe central, northwestern and western Anatolian magmatic provinces are defined by a large number of late Mesozoic to late Cenozoic collision-related granitoids. Calc-alkaline, subalkaline and alkaline intrusive rocks in central Anatolia are mainly metaluminous, shoshonitic, I- to A-types. They cover a petrological range from monzodiorite through quartz monzonite to granite/syenite, and are all enriched in LILE. Their geochemical characteristics are consistent with formation from a subduction-modified mantle source. Calc-alkaline plutonic rocks in northwestern Anatolia are mainly metaluminous, medium- to high-K and I-types. They are monzonite to granite, and all are enriched in LILE and depleted in HFSE, showing features of arc-related intrusive rocks. Geochemical data reveal that these plutons were derived from partial melting of mafic lower crustal sources. Calc-alkaline intrusive rocks in western Anatolia are metaluminous, high-K and I-types. They have a compositional range from granodiorite to granite, and are enriched in LILE and depleted in HFSE. Geochemical characteristics of these intrusive rocks indicate that they could have originated by the partial melting of mafic lower crustal source rocks.en_US
dc.identifier.doi10.1080/00206810802673933
dc.identifier.endpage278en_US
dc.identifier.issn0020-6814
dc.identifier.issue3en_US
dc.identifier.scopus2-s2.0-75649142111en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage252en_US
dc.identifier.urihttps://doi.org/10.1080/00206810802673933
dc.identifier.urihttps://hdl.handle.net/20.500.12483/8484
dc.identifier.volume51en_US
dc.identifier.wosWOS:000264824500003en_US
dc.identifier.wosqualityQ1en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_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.subjectcalc-alkalineen_US
dc.subjectsubalkalineen_US
dc.subjectgraniteen_US
dc.subjectcollision-relateden_US
dc.subjectlower crusten_US
dc.subjectAnatoliaen_US
dc.titleCollision-related granite magma genesis, potential sources and tectono-magmatic evolution: comparison between central, northwestern and western Anatolia (Turkey)en_US
dc.typeReview Articleen_US

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