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dc.contributor.authorYıldız, Ahmet
dc.contributor.authorKibici, Yaşar
dc.contributor.authorBağcı, Metin
dc.contributor.authorDumlupunar, İbrahim
dc.contributor.authorKocabaş, Cumhur
dc.contributor.authorArıtan, Ali Ekrem
dc.date.accessioned2019-10-17T06:44:43Z
dc.date.available2019-10-17T06:44:43Z
dc.date.issued2015en_US
dc.identifier.issn1866-7511
dc.identifier.issn1866-7538
dc.identifier.urihttps://doi.org/10.1007/s12517-015-1991-4
dc.identifier.urihttps://hdl.handle.net/20.500.12462/7360
dc.descriptionKocabaş, Cumhur (Balikesir Author)en_US
dc.description.abstractEocene volcanic rocks from the Central Sakarya Zone in the north of the A degrees zmir-Ankara suture zone (IASZ) are predominantly intermediate-acidic lava flows and pyroclastics that crop out with a W-E orientation. The volcanic rocks include Bozani double dagger lavas, agglomerates, A degrees AYdir lavas, and KapA +/- kaya tuffs. The Bozani double dagger lavas contain plagioclase, hornblende, clinopyroxene, and biotite, whereas the A degrees AYdir lavas consist of plagioclase, hornblende, biotite, and quartz. According to the total alkali-silica (TAS) diagram, the Bozani double dagger lavas are mainly composed of andesite and dacite, with one sample of trachyandesite, whereas the A degrees AYdir lavas mainly contain dacite and minor andesite. Bozani double dagger and A degrees AYdir lavas exhibit moderate- to high-K calc-alkaline character. Major oxide and trace element variations suggest the effects of fractional crystallization in the evolution of the volcanic rocks. N-type mid-ocean ridge basalt (MORB) normalized trace element patterns of the lavas exhibit enrichment in large ion lithophile elements (LILEs; K, Rb, Ba, Th) and depletion in high field strength elements (HFSEs; Zr, Ti, Y). In addition, the chondrite-normalized rare earth element (REE) plots of the rocks show moderately enriched and nearly concave-shaped patterns (La-N/Yb-N = 5.4-17.6 for the Bozani double dagger lavas and 6.5-13.1 for the A degrees AYdir lavas), suggesting clinopyroxene (Cpx) and hornblende dominated fractionation. Negative Eu anomalies in the acidic lavas reveal plagioclase fractionation. Some trace element ratios of the lavas demonstrate a subduction signature and crustal contamination in the generation of the parent magma(s). Multi-dimensional tectonic discrimination diagrams suggest that the studied volcanic rocks have developed in a collisional setting.en_US
dc.description.sponsorshipScientific and Technical Research Council of Turkey (TUBITAK)en_US
dc.language.isoengen_US
dc.publisherSpringer Heidelbergen_US
dc.relation.isversionof10.1007/s12517-015-1991-4en_US
dc.rightsinfo:eu-repo/semantics/embargoedAccessen_US
dc.subjectPost-collisionen_US
dc.subjectVolcanismen_US
dc.subjectCalc-alkalineen_US
dc.subjectSakarya Continenten_US
dc.subjectTurkeyen_US
dc.titlePetrogenesis of the post-collisional Eocene volcanic rocks from the Central Sakarya Zone (Northwestern Anatolia, Turkey): Implications for source characteristics, magma evolution, and tectonic settingen_US
dc.typearticleen_US
dc.relation.journalArabian Journal of Geosciencesen_US
dc.contributor.departmentMühendislik-Mimarlık Fakültesien_US
dc.contributor.authorID0000-0002-1056-2854en_US
dc.contributor.authorID0000-0002-4967-3877en_US
dc.identifier.volume8en_US
dc.identifier.issue12en_US
dc.identifier.startpage11239en_US
dc.identifier.endpage11260en_US
dc.relation.tubitakinfo:eu-repo/grantAgreement/TUBITAK/104Y160en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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