Mineralogy, fluid inclusion and stable isotope characteristics of the Inlice (Konya, Turkey) high sulfidation epithermal gold deposit: Implications for hydrothermal evolution and ore genesis

dc.contributor.authorTerzi, Mustafa Haydar
dc.contributor.authorYılmazer, Erkan
dc.contributor.authorKuşcu, İlkay
dc.contributor.authorOyman, Tolga
dc.contributor.authorBozan, Sercan
dc.date.accessioned2024-07-09T07:01:51Z
dc.date.available2024-07-09T07:01:51Z
dc.date.issued2024
dc.departmentMühendislik Fakültesi
dc.description.abstractThe Inlice high sulfidation epithermal gold deposit with 262,300 oz of gold ore is located in the Erenlerdağ-Alacadağ Volcanic Complex (EAVC) at the northern part of central Taurides. The volcanic succession of the study area is stratigraphically represented by andesite, block and ash flow, basaltic andesite lava flow and andesite lava flow. The deposit consists of seven neighboring mineralized veins termed Ana East, Ana West, West, Discovery, Güllü, Merkez and North Zone and is associated with an andesite (ca 8–9 Ma). Hydrothermal alteration from the innermost to the outermost parts of the deposit includes silicification, advanced argillic, intermediate argillic and propylitic. At the surface, quartz veins related to silicification are exposed as linear topographic relief trending mainly northwest-southeast and secondarily northeast-southwest and east-west. Deep drill core samples, including magnetite, quartz, biotite and anhydrite, imply the presence of potassic alteration in depth (50 to 970 m) possibly related to a porphyry Cu system. Ore assemblages are described as hypogene and supergene. The hypogene ore mainly includes pyrite (Py-I and Py-II) and enargite, and to a lesser extent chalcopyrite, sphalerite and marcasite. The supergene ore incorporates hematite and goethite, and minor covellite, chalcocite, malachite and native copper. Hypogene gold precipitation is associated with the mineral association of Py-II, chalcopyrite and enargite, while enargite mineral is a major host for gold (up to 600 ppm). Supergene oxidation resulted in the development of a secondary enrichment zone for gold (up to 14 g/t) extending to a depth of about 45 m. Microthermometric measurements show that the silicification associated with the mineralization was formed at homogenization temperatures ranging between 147 and 360 °C and salinities up to 6.5 wt% NaCl. This suggests that the fluid mixing and/or fluid dilution processes were important factors controlling the precipitation of gold. ?34S isotope compositions are between ?0.9 and ? 9 ‰, and further indicate a significant involvement of magmatic components into the hydrothermal fluids. Thus, it is concluded that at Inlice the hydrothermal fluids responsible for the alteration and mineralization processes were derived by relatively dilute fluids formed by the mixing of magmatic fluids with meteoric waters.
dc.identifier.doi10.1016/j.chemer.2023.126040
dc.identifier.issn0009-2819
dc.identifier.issue1en_US
dc.identifier.scopusqualityQ1
dc.identifier.urihttps:/dx.doi.org/10.1016/j.chemer.2023.126040
dc.identifier.urihttps://hdl.handle.net/20.500.12451/12092
dc.identifier.volume84en_US
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherElsevier GmbH
dc.relation.ispartofGeochemistry
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/embargoedAccess
dc.subjectEpithermal
dc.subjectFluid Inclusions
dc.subjectGold
dc.subjectHigh Sulfidation
dc.subjectInlice
dc.subjectMineral Chemistry
dc.subjectSulphur Isotopes
dc.subjectTurkey
dc.titleMineralogy, fluid inclusion and stable isotope characteristics of the Inlice (Konya, Turkey) high sulfidation epithermal gold deposit: Implications for hydrothermal evolution and ore genesis
dc.typeArticle

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