Petrogenesis of the uckapl Granitoid and its Mafic Enclaves in Elmal Area (Nide, Central Anatolia, Turkey)

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dc.contributor.authorKurt, Huseyin
dc.contributor.authorKocak, Kerim
dc.contributor.authorAsan, Kursad
dc.contributor.authorKarakas, Mustafa
dc.date.accessioned2020-03-26T18:42:51Z
dc.date.available2020-03-26T18:42:51Z
dc.date.issued2013
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractThe Late Cretaceous uckapl Granitoid including mafic microgranular enclaves intruded into metapelitic and metabasic rocks, and overlain unconformably by Neogene ignimbrites in the Nigde area of Turkey. It is mostly granite and minor granodiorite in composition, whereas its enclaves are dominantly gabbro with a few diorites in composition. The uckapl Granitoid is composed mainly of quartz, K-feldspar, plagioclase, biotite, muscovite and minor amphibole while its enclaves contain mostly plagioclase, amphibole, minor pyroxene and biotite. The uckapl Granitoid has calcalkaline and peraluminous (A/CNK= 1.0-1.3) geochemical characteristics. It is characterized by high LILE/HFSE and LREE/HREE ratios ((La/Lu)(N)= 3-33), and has negative Ba, Ta, Nb and Eu anomalies, resembling those of collision granitoids. The uckapl Granitoid has relatively high (SrSr(i))-Sr-87-Sr-86 ratios (0.711189-0.716061) and low epsilon Nd-(t) values (-5.13 to -7.13), confirming crustal melting. In contrast, the enclaves are tholeiitic and metaluminous, and slightly enriched in LILEs (K, Rb) and Th, and have negative Ta, Nb and Ti anomalies; propose that they were derived from a subduction-modified mantle source. Based on mineral and whole rock chemistry data, the uckapl granitoid is H-(hybrid) type, post-collision granitoid developed by mixing/mingling processes between crustal melts and mantle-derived mafic magmas.en_US
dc.description.sponsorshipSelcuk UniversitySelcuk University [2004/37]en_US
dc.description.sponsorshipThis study was financially supported by the Selcuk University Scientific Research Projects Coordination (Project No: 2004/37). The authors gratefully thank the Selcuk University for its support. The authors also thank editor in chief Dr. Fei Hongcai and anonymous reviewers for critical and constructive comments.en_US
dc.identifier.doi10.1111/1755-6724.12085en_US
dc.identifier.endpage748en_US
dc.identifier.issn1000-9515en_US
dc.identifier.issn1755-6724en_US
dc.identifier.issue3en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.startpage738en_US
dc.identifier.urihttps://dx.doi.org/10.1111/1755-6724.12085
dc.identifier.urihttps://hdl.handle.net/20.500.12395/29721
dc.identifier.volume87en_US
dc.identifier.wosWOS:000321845300011en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherWILEYen_US
dc.relation.ispartofACTA GEOLOGICA SINICA-ENGLISH EDITIONen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectH-type granitoiden_US
dc.subjectmafic enclaveen_US
dc.subjectgeochemistryen_US
dc.subjectCentral Anatoliaen_US
dc.subjectTurkeyen_US
dc.titlePetrogenesis of the uckapl Granitoid and its Mafic Enclaves in Elmal Area (Nide, Central Anatolia, Turkey)en_US
dc.typeArticleen_US

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