Geochemical constraints on the genesis of the Gunyuzu pluton, northwest Anatolia, Turkey

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dc.authoridIlbeyli, Nurdane/0000-0002-0557-8771
dc.contributor.authorKibici, Yasar
dc.contributor.authorIlbeyli, Nurdane
dc.contributor.authorYildiz, Ahmet
dc.contributor.authorBagci, Metin
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.abstractTavsanli Zone in northwest Turkey is intruded by many Late Cretaceous to Eocene (91-45 Ma) calc-alkaline granitoids, of which the Gunyuzu pluton in the Eskisehir region is the least studied. The Gunyuzu rocks are high-K, calc-alkaline (I-type) intrusions. and are comprised of diorite, granodiorite, granite, and granite porphyry. Typical minerals are plagioclase, K-feldspar, quartz, biotite, hornblende and Fe-Ti oxides. Chondrite-normalized REE patterns for the Gunyuzu rocks are moderately fractionated and have small negative Eu anomalies. They are enriched in LILE and LREE relative to HFSL, showing characteristics of arc-related granitoids. Low values of molar K2O/Na2O, Al2O3/(FeO+MgO+TiO2). and (Na2O+K2O)/(FeO+MgO+TiO2) ratios demonstrate that the Gunyuzu magma(s) were produced from mafic lower crustal rocks.en_US
dc.description.sponsorshipAfyon Kocatepe Universityen_US
dc.description.sponsorshipThe research was supported by Afyon Kocatepe University in every phase of this study. We are also grateful Afyon Kocatepe University for providing a research car during field work. Dr. Selman Aydogan is thanked for assistance during the field and also supplied some figures. We specially thank to Prof. Dr. Donna L. Whitney for her constructive and detailed review of this manuscript.en_US
dc.identifier.doi10.2747/0020-6814.50.10.931
dc.identifier.endpage947en_US
dc.identifier.issn0020-6814
dc.identifier.issn1938-2839
dc.identifier.issue10en_US
dc.identifier.scopus2-s2.0-65649146141en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage931en_US
dc.identifier.urihttps://doi.org/10.2747/0020-6814.50.10.931
dc.identifier.urihttps://hdl.handle.net/20.500.12483/13731
dc.identifier.volume50en_US
dc.identifier.wosWOS:000259154700005en_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.subjectMagmatic Complexen_US
dc.subjectWesternen_US
dc.subjectEvolutionen_US
dc.subjectGenerationen_US
dc.subjectGranitoidsen_US
dc.subjectRocksen_US
dc.subjectZoneen_US
dc.subjectGeochronologyen_US
dc.subjectPetrogenesisen_US
dc.subjectMetamorphismen_US
dc.titleGeochemical constraints on the genesis of the Gunyuzu pluton, northwest Anatolia, Turkeyen_US
dc.typeArticleen_US

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