Fluid inclusion and sulfur isotope thermometry of the Inkaya (Simav-Kutahya) Cu-Pb-Zn-(Ag) mineralization, NW TURKEY

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dc.contributor.authorOzen, Yesim
dc.contributor.authorArik, Fetullah
dc.date.accessioned2020-03-26T18:42:00Z
dc.date.available2020-03-26T18:42:00Z
dc.date.issued2013
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractThe Inkaya Cu-Pb-Zn-(Ag) mineralization, located about 20 km west of the Simav (Kutahya-Turkey), is situated in the northern part of the Menderes Massif Metamorphics. The mineralization is located along an E-W trending fault in the Cambrian Simav metamorphics consisting of quartz-muscovite schist, quartz-biotite schist, muscovite schist, biotite schist and the ArA +/- kayasA +/- formation composed of marbles. Mineralized veins are 30-35 cm in width. The primary mineralization is represented by abundant galena, sphalerite, chalcopyrite, pyrite, fahlore and minor amounts of cerussite, anglesite, digenite, enargite, chalcocite, covellite, bornite, limonite, hematite and goethite with gangue quartz. Fluid inclusion studies on the quartz samples collected from the mineralized veins indicate that the temperature range of the fluids is 235A degrees C to 340A degrees C and the salinities are 0.7 to 4.49 wt. % NaCl equivalent. The wide range of homogenization temperatures indicates that two different fluid generations were trapped in quartz. Sulfur isotope studies of the sulfide minerals showed that all of the delta S-34 values are between -2.1 and 2.6 per mil. These values are a typical range for hydrothermal sulfide minerals that have sulfur derived from a magmatic source. Pyrite-galena and pyrite-chalcopyrite sulfur isotope fractionation is consistent with an approach to isotopic equilibrium, and calculated temperatures are 254.6 and 277.4A degrees C for pyrite-galena and 274.7A degrees C for pyrite-chalcopyrite. The microthermometric data and sulfur isotope thermometry indicate the existence of a hydrothermal fluid that circulated along the fault crossing the Simav metamorphics and ArA +/- kayasA +/- formation. Fluid inclusion and sulfur isotope thermometry can be used in combination with ore petrographical and geological information to provide site-specific targets for meso-hypothermal metal concentrations.en_US
dc.description.sponsorshipScientific Research Project Coordination of Selcuk University (BAP)Selcuk University [09101029, 09401059]; TUBITAK-CAYDAGTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [110Y355]en_US
dc.description.sponsorshipThe authors wish to thank Prof. Dr. Ilkay KUSCU (Mugla Sitki Kocman University-Mugla-TURKEY), Prof. Dr. Nilgun GULEC (Middle East Technical University-METU-Ankara-TURKEY), Asst. Prof. Dr. Nurullah HANILCI (Istanbul University-Istanbul-TURKEY) and Prof. Dr. Ibrahim COPUROGLU (Nigde University-Nigde-TURKEY) for their helpful discussions, advice and encouragement. The authors would like to thank reviewers for their careful reading of the paper and their helpful comments. This paper that is part of the PhD research has been supported by Scientific Research Project Coordination of Selcuk University (BAP Project No: 09101029 and 09401059) and TUBITAK-CAYDAG (Project No: 110Y355).en_US
dc.identifier.doi10.2478/s13533-012-0139-2en_US
dc.identifier.endpage449en_US
dc.identifier.issn2081-9900en_US
dc.identifier.issn1896-1517en_US
dc.identifier.issue3en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage435en_US
dc.identifier.urihttps://dx.doi.org/10.2478/s13533-012-0139-2
dc.identifier.urihttps://hdl.handle.net/20.500.12395/29526
dc.identifier.volume5en_US
dc.identifier.wosWOS:000325174100009en_US
dc.identifier.wosqualityQ4en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherDE GRUYTER OPEN LTDen_US
dc.relation.ispartofCENTRAL EUROPEAN JOURNAL OF GEOSCIENCESen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectFluid inclusionen_US
dc.subjectsulfur isotope thermometryen_US
dc.subjectInkaya Cu-Pb-Zn-(Ag) mineralizationen_US
dc.subjectSimaven_US
dc.subjectmeso-hypothermalen_US
dc.titleFluid inclusion and sulfur isotope thermometry of the Inkaya (Simav-Kutahya) Cu-Pb-Zn-(Ag) mineralization, NW TURKEYen_US
dc.typeArticleen_US

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