Petrogenesis of the Late Cenozoic Egrigoz pluton in western Anatolia, Turkey: implications for magma genesis and crustal processes

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dc.authoridIlbeyli, Nurdane/0000-0002-0557-8771
dc.contributor.authorOzgenc, Ismet
dc.contributor.authorIlbeyli, Nurdane
dc.date.accessioned2024-09-18T21:06:37Z
dc.date.available2024-09-18T21:06:37Z
dc.date.issued2008
dc.departmentHatay Mustafa Kemal Üniversitesien_US
dc.description.abstractThe western Anatolian magmatic province is typified by a large number of Late Cenozoic post-collisional granitoids. Of these magmatics, the Egrigoz pluton is one of the largest and least-understood plutons in the Menderes Massif. The Egrigoz intrusives are subalkaline, high-K, and calc-alkaline, and have characteristics of I-type granites. They consist mainly of granodiorite and granite. The intrusive rocks show enrichment in LILE and LREE relative to HFSE. Their chondrit-enormalized REE patterns are fractionated and have small negative Eu anomalies. Geochemical characteristics of the Egrigoz pluton indicate an origin through partial melting of mafic lower-crustal source rocks. In western Anatolia, the melt generation mechanism for the intrusive rocks could be crustal extension and uplift following collision.en_US
dc.identifier.doi10.2747/0020-6814.50.4.375
dc.identifier.endpage391en_US
dc.identifier.issn0020-6814
dc.identifier.issue4en_US
dc.identifier.scopus2-s2.0-42549086813en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage375en_US
dc.identifier.urihttps://doi.org/10.2747/0020-6814.50.4.375
dc.identifier.urihttps://hdl.handle.net/20.500.12483/13732
dc.identifier.volume50en_US
dc.identifier.wosWOS:000254558000003en_US
dc.identifier.wosqualityQ2en_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.subjectSouthern Menderes Massifen_US
dc.subjectI-Type Granitoidsen_US
dc.subjectCore-Complexen_US
dc.subjectGeochemical Constraintsen_US
dc.subjectNorthwestern Anatoliaen_US
dc.subjectTectonic Significanceen_US
dc.subjectGeodynamic Evolutionen_US
dc.subjectContinental-Crusten_US
dc.subjectAugen Gneissesen_US
dc.subjectSw Turkeyen_US
dc.titlePetrogenesis of the Late Cenozoic Egrigoz pluton in western Anatolia, Turkey: implications for magma genesis and crustal processesen_US
dc.typeArticleen_US

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