Geochemical constraints on the genesis of the Saricakaya intrusive rocks, Turkey: Late Paleozoic crustal melting in the central Sakarya Zone

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dc.authoridIlbeyli, Nurdane/0000-0002-0557-8771
dc.contributor.authorKibici, Y.
dc.contributor.authorIlbeyli, N.
dc.contributor.authorYildiz, A.
dc.contributor.authorBagci, M.
dc.date.accessioned2024-09-18T19:54:18Z
dc.date.available2024-09-18T19:54:18Z
dc.date.issued2010
dc.departmentHatay Mustafa Kemal Üniversitesien_US
dc.description.abstractThe Sakarya Zone is intruded by several Late Paleozoic granitoids, of which the Saricakaya intrusive rocks in the central Sakarya (Eskisehir) region, is the least-studied. The Saricakaya intrusive rocks consist mainly of quartz diorite-granodiorite, granodiorite and granite. They are, geochemically, divided into two groups: diorites and granites. The former is medium-K and calc-alkaline (mainly l-type), whereas the latter is high-K to shoshonite and calcic (I-type). Typical minerals for both rock types are plagioclase, K-feldspar, quartz, biotite, hornblende and Fe-Ti oxides. Chondrite-normalized REE patterns for the Saricakaya intrusive rocks are moderately fractionated and have small negative Eu anomalies. They are enriched in LILE and LREE relative to HFSE showing characteristics of arc-related granitoids. Geochemical characteristics of the Saricakaya intrusive rocks indicate a hybrid origin through partial melting of lower crustal source rocks. (C) 2010 Elsevier GmbH. All rights reserved.en_US
dc.identifier.doi10.1016/j.chemer.2009.12.001
dc.identifier.endpage256en_US
dc.identifier.issn0009-2819
dc.identifier.issn1611-5864
dc.identifier.issue3en_US
dc.identifier.scopus2-s2.0-77955327488en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage243en_US
dc.identifier.urihttps://doi.org/10.1016/j.chemer.2009.12.001
dc.identifier.urihttps://hdl.handle.net/20.500.12483/7646
dc.identifier.volume70en_US
dc.identifier.wosWOS:000281998600003en_US
dc.identifier.wosqualityQ2en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherElsevier Gmbh, Urban & Fischer Verlagen_US
dc.relation.ispartofChemie Der Erde-Geochemistryen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectAnatoliaen_US
dc.subjectCentral Sakaryaen_US
dc.subjectSaricakayaen_US
dc.subjectI-type graniteen_US
dc.subjectLower crusten_US
dc.subjectMeltingen_US
dc.titleGeochemical constraints on the genesis of the Saricakaya intrusive rocks, Turkey: Late Paleozoic crustal melting in the central Sakarya Zoneen_US
dc.typeArticleen_US

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