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dc.contributor.authorKaygusuz, Abdullah
dc.contributor.authorOzturk, Mursit
dc.date.accessioned2021-11-09T19:42:19Z
dc.date.available2021-11-09T19:42:19Z
dc.date.issued2015
dc.identifier.issn1367-9120
dc.identifier.issn1878-5786
dc.identifier.urihttps://doi.org/10.1016/j.jseaes.2015.04.017
dc.identifier.urihttps://hdl.handle.net/20.500.12440/3340
dc.description.abstractEocene I-type plutons are widespread in the Eastern Pontides, Northeastern Turkey. Geochemical and isotopic results on two Eocene intrusive bodies located in the southern zone of the Eastern Pontides were utilized to achieve a proper reconstruction of their origin. Based on laser ablation ICP-MS U-Pb zircon dating, Kilickaya and Kozluk intrusions present similar Pb-206/U-238 versus Pb-207/U-235 concordia ages of 46.75 +/- 0.79 and 46.9 +/- 0.68 Ma, respectively. Both intrusions exhibit similar petrographical, geochemical, and isotopical features, and contain abundant mafic microgranular enclaves (MMEs). The intrusive rocks are composed of diorite, tonalite, and granodiorite, whereas MMEs are composed of diorite. Both the intrusive rocks and the MMEs are I-type, high-K calc-alkaline in composition and display a metaluminous character. They are enriched in large-ion lithophile and light rare-earth elements and are depleted in high-field strength elements. The intrusive rocks show moderate variation in Sr-87/Sr-86(I) (0.70531-0.70576), epsilon Nd-(i) (+03 to -0.5), and delta O-18 values (+6.6 to +6.9), as well as Nd model ages (0.73-0.82 Ga). Their Pb isotopic ratios are Pb-206/Pb-204 = 18.67-18.86, (207)pb/(204)pb = 15.61-15.62, and (208)pb/(204)pb = 38.62-39.03. Although the isotope signatures of MMEs (Sr-87/Sr-86((i)) = 0.70528-0.70561; epsilon Nd-(i)= +0.7 to -0.3; delta O-18 = +6.7 to +6.8) are significantly similar to those of the host rocks, the MMEs are characterized by relatively low contents of SiO2 (57-59 wt.%), low aluminum saturation index (0.8-0.9), and high Mg numbers (31-36). All of these data suggest magma generation by mixing of enriched lithospheric mantle- and lower crustal-derived melts. Moreover, Sr-Nd isotopic modeling reveals similar to 17% to 23% lower crustal magma contribution to the mantle component. (C) 2015 Elsevier Ltd. All rights reserved.en_US
dc.description.sponsorshipScientific Research Projects Foundation of Gumushane UniversityGumushane University [2013.F5114.02.01]en_US
dc.description.sponsorshipThis work was financially supported by the Scientific Research Projects Foundation of Gumushane University (Project No.: 2013.F5114.02.01). We thank Frank C. Ramos and Kurt Kyser for providing Sr-Nd-Pb and oxygen isotopic analyses, as well as Bin Chen for help during U-Pb zircon dating. Thanks are due to Bor-Ming Jahn for editorial handling, Siebel Wolfgang and two anonymous reviewers for their general improvement of the manuscript. Gokhan Cakmak and Metin Ciftci are also thanked for their help during the fieldwork.en_US
dc.language.isoengen_US
dc.publisherPergamon-Elsevier Science Ltden_US
dc.relation.ispartofJournal of Asian Earth Sciencesen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectEocene magmatismen_US
dc.subjectSr-Nd-Pb-O isotopeen_US
dc.subjectU-Pb zircon datingen_US
dc.subjectEastern Pontidesen_US
dc.subjectTurkeyen_US
dc.titleGeochronology, geochemistry, and petrogenesis of the Eocene Bayburt intrusions, Eastern Pontides, NE Turkey: Evidence for lithospheric mantle and lower crustal sources in the high-K calc-alkaline magmatismen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.description.wospublicationidWOS:000358101100008en_US
dc.description.scopuspublicationid2-s2.0-84928897670en_US
dc.departmentGümüşhane Üniversitesien_US
dc.identifier.volume108en_US
dc.identifier.startpage97en_US
dc.identifier.doi10.1016/j.jseaes.2015.04.017
dc.identifier.endpage116en_US
dc.authorwosid, Abdullah / Q-2029-2015
dc.authorscopusid6701580075
dc.authorscopusid56622262300


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