Fingerprint of magma mixture in the leucogranites: Spectroscopic and petrochemical approach, Kalebalta-Central Anatolia, Türkiye

dc.contributor.authorGüllü, Bahattin
dc.contributor.authorAkşit, Asuman
dc.date.accessioned2024-04-22T05:56:46Z
dc.date.available2024-04-22T05:56:46Z
dc.date.issued2023
dc.departmentMühendislik Fakültesi
dc.description.abstractLeucogranites of Kalebalta in Central Anatolia are composed of plagioclase, quartz, orthoclase, and biotite and contains mafic microgranular enclaves (MME) in sizes ranging from few cm to 70 cm. In the total alkali-silica diagram, they fall typically in the granite field and show a calc-alkaline nature in the alkalis-iron-magnesium diagram whereas enclaves are Medium K series calc-alkaline, which represents the transition from tholeiitic to calc-alkaline. Leucogranites which have A/CNK(mol%) > 1 are strong peraluminous and seen as the products of magma derived from a metasedimentary source. Signs of magma mixing expressing the mantle inputs are also observed in many bivariation diagrams. Zircon and apatite saturation temperatures calculated on the basis of whole rock chemistry are 744-829°C for leucogranites and 761-832°C for their enclaves. According to the Raman spectra, biotite and plagioclase minerals in leucogranites and their enclaves show similar Raman spectrums. The biotite minerals have Mg-O and/or Fe-O translational (transformation) bonds between 182 and 552 cm-1, Si-O-Si bending between 552 and 1,100 cm-1 and Si-O-Si vibrational bonds between 1,100 and 1,200 cm-1. The results of this study suggest that the leucogranites and enclaves are most probably derived from different magmas. In addition, according to geochemical and spectroscopic data, they may also have fractional crystallization, which is effective after the mixing process.
dc.identifier.doi10.1515/geo-2022-0548
dc.identifier.issn2391-5447
dc.identifier.issue1en_US
dc.identifier.scopusqualityQ2
dc.identifier.urihttps:/dx.doi.org10.1515/geo-2022-0548
dc.identifier.urihttps://hdl.handle.net/20.500.12451/11670
dc.identifier.volume15en_US
dc.identifier.wosWOS:001083960300001
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherWalter de Gruyter GmbH
dc.relation.ispartofOpen Geosciences
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectLeucogranites
dc.subjectMafic Microgranular Enclave
dc.subjectMantle Input
dc.titleFingerprint of magma mixture in the leucogranites: Spectroscopic and petrochemical approach, Kalebalta-Central Anatolia, Türkiye
dc.typeArticle

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