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dc.contributor.authorKarakuş, Hüseyin
dc.contributor.authorErgüler, Zeynal Abiddin
dc.contributor.authorÖzkul, Cafer
dc.contributor.authorYanık, Gürsel
dc.contributor.authorKibici, Yaşar
dc.date.accessioned2019-07-12T06:41:31Z
dc.date.available2019-07-12T06:41:31Z
dc.date.issued2019en_US
dc.identifier.citationKarakuş, H., Ergüler, Z. A., Özkul, C., Yanık, G., & Kibici, Y. (2019). Geochemical and isotopic characteristics of geothermal discharges in the Emet Basin, Western Anatolia, Turkey. Applied Geochemistry.en_US
dc.identifier.urihttps://doi.org/10.1016/j.apgeochem.2019.06.002
dc.identifier.urihttps://hdl.handle.net/20.500.12438/570
dc.description.abstractThe geochemical and isotopic compositions of low-temperature thermal waters in the N–S-oriented Emet Basin, located in Western Anatolia, Turkey, were comprehensively investigated. Three distinct physicochemical processes affecting the chemical composition of the thermal waters were distinguished at this site: dissolution of CaCO3, gradual transformation of Ca–HCO3-type waters to Ca–SO4-type waters by the addition of SO4, and mixing of deep Na–HCO3-type waters with Ca–SO4-type waters. The first two processes are associated with the dissolution of carbonates and evaporites, respectively, and predominantly control the chemistry of thermal waters in the basin. The third process is observed locally and is manifested as CO2-rich thermal waters with relatively higher total ionic concentration. The majority of the thermal waters lie close to the local meteoric water line with a deuterium excess of +17‰. The single CO2-rich thermal water in the basin, located in the Yeniceköy area, shows a slight enrichment in 18O and a shift from the local meteoric water line. The δ34SSO4 and δ18OSO4 values of the dissolved sulfate range from 14.49‰ to 22.46‰ (vs. V-CDT) and 11.9‰–17.8‰ (vs. V-SMOW), respectively, which indicates that the source of sulfate in the thermal waters is evaporites such as gypsum and anhydrite in the basin. The δ13CDIC values of the thermal waters vary between −0.63‰ and −10.36‰ (vs. V-PDB). By using a binary mixing model, the δ13C value of the deep carbon source associated with the formation of CO2-rich thermal waters was calculated as 0‰, which is a typical value of marine limestones. Thermal decomposition of marine limestones and dissolution of carbonates dominate the carbon budgets of thermal waters, whereas the organic carbon contribution is generally less than 20% and the mantle-derived carbon contribution was found to be insignificant. Air-corrected 3He/4He ratios of the thermal waters ranging from 0.34 RA to 1.57 RA indicate that radiogenic (crustal) helium is dominant in the region, although up to 19.4% of the total helium is of mantle origin. The 3He/heat ratios vary from 0.4 × 10−15 cm3 STP/J to 13.2 × 10−15 cm3 STP/J, which are very close to the ratios in the continental environment. This indicates that the dominant heat source in the region is radiogenic. © 2019 Elsevier Ltden_US
dc.language.isoengen_US
dc.publisherElsevieren_US
dc.relation.isversionof10.1016/j.apgeochem.2019.06.002en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_us
dc.subjectEmeten_US
dc.subjectGeothermalen_US
dc.subjectGeochemistryen_US
dc.subjectIsotopeen_US
dc.subjectHeliumen_US
dc.titleGeochemical and isotopic characteristics of geothermal discharges in the Emet Basin, Western Anatolia, Turkeyen_US
dc.typearticleen_US
dc.relation.journalApplied Geochemistryen_US
dc.departmentMühendislik Fakültesien_US
dc.contributor.authorIDhttp://orcid.org/0000-0002-9060-7265en_US
dc.contributor.authorIDhttp://orcid.org/0000-0003-2785-1967en_US
dc.identifier.volume107en_US
dc.identifier.startpage105en_US
dc.identifier.endpage119en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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