Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.13091/783
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dc.contributor.authorÇelik Karakaya, Muazzez-
dc.contributor.authorBozdağ, Ayla-
dc.contributor.authorÜnal Ercan, Hatice-
dc.contributor.authorKarakaya, Necati-
dc.contributor.authorDelikan, Arif-
dc.date.accessioned2021-12-13T10:29:58Z-
dc.date.available2021-12-13T10:29:58Z-
dc.date.issued2019-
dc.identifier.issn0375-6742-
dc.identifier.issn1879-1689-
dc.identifier.urihttps://doi.org/10.1016/j.gexplo.2019.03.004-
dc.identifier.urihttps://hdl.handle.net/20.500.13091/783-
dc.description.abstractThe study area is located in the south of Konya Closed Basin which is the largest Miocene inner basin in Central Anatolia. The aim of this study is to determine the chemical composition of the Miocene halite deposits and depositional environments of Tuz Golu lacustrine basin. For this scope, fluid inclusion analyses (K+, Mg2+, SO42-) of nine pure halites were performed and twenty six pure halite samples have been examined. Additionally, K+, Mg2+, SO42- ion concentrations of the fluid inclusions and pure halite samples were compared to Gulf of Suez (GS), Red Sea (RS) and other Cenozoic seawaters (CS). Results from analyses show that K+ content of the fluid inclusions of the halites in the Tuz Golu basin, which are considerably higher than the K+ contents both of the pure halites and the GS and RS and CS, result from dissolution of the primary K+-salts. The Br-content of the pure halite samples is ranging from 5 to 637 ppm. The high Br-(> 40 ppm) content indicates the marine origin while the low Br-content is related to dissolution and recycled of the previously deposited marine halites. Mg2+ and SO42- contents of the Tuz Golu basin samples are higher than those of the GS and RS and CS except for TG4 samples. The high Mg2+ and SO42- contents were resulted from the dissolution of previously deposited gypsum and de-dolomitization process. delta S-34 isotope (18.80 to 21.00 parts per thousand) and low delta O-18 (8.10 to 9.50 parts per thousand) values of the Tuz Golu basin samples, which are compatible with isotope values of the CS, indicate marine origin. In addition, the high delta O-18 values (16.20 to 20.50 parts per thousand) and the delta S-34 content can be explained by recycling of marine sulphate as well as dissolution and re-crystalization of previously deposited sulphates. The possible effective mechanisms causing chemical differences in the Tuz Golu basin, which is a sedimentary basin formed under highly complex different physico-chemical mechanisms, have been detected as (1) the changes in chemistry of halites due to dissolution and re-crystallization processes of previously deposited halites and evaporites, (2) de-dolomitization processes and (3) seawater input.en_US
dc.description.sponsorshipScientific and Technological Research Council of TurkeyTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [TUBITAK 114Y629]; Selcuk University Scientific Research Projects support programSelcuk University [SUBAP16401034]en_US
dc.description.sponsorshipThis research was made possible with the support of The Scientific and Technological Research Council of Turkey (TUBITAK 114Y629) and partly the Selcuk University Scientific Research Projects support program (SUBAP16401034). We would like to thank Prof. Dr. Krzysztof Bukowski and Dr. Anatoliy R. Galamay for their contribution to fluid inclusions analyzes in AGH laboratories of Poland and also for their contribution to the interpretation of fluid inclusions. Thanks to Dr. Tom Hill and the National History Museum for their scientific supports in microfossils studies. We also thanks to MTA helping us to get the drilling samples.en_US
dc.language.isoenen_US
dc.publisherELSEVIER SCIENCE BVen_US
dc.relation.ispartofJOURNAL OF GEOCHEMICAL EXPLORATIONen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectTuz Golu Basinen_US
dc.subjectHaliteen_US
dc.subjectFluid Inclusionen_US
dc.subjectDissolution-Re-Crystalizationen_US
dc.subjectDe-Dolomitizationen_US
dc.subjectSeawater Chemistryen_US
dc.subjectSecular Variationen_US
dc.subjectSalt Lakeen_US
dc.subjectMarineen_US
dc.subjectEvolutionen_US
dc.subjectSulfuren_US
dc.subjectSulfateen_US
dc.subjectOxygenen_US
dc.subjectZoneen_US
dc.subjectSuezen_US
dc.titleOrigin of Miocene halite from Tuz Golu basin in Central Anatolia, Turkey: Evidences from the pure halite and fluid inclusion geochemistryen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.gexplo.2019.03.004-
dc.identifier.scopus2-s2.0-85063691408en_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeoloji Mühendisliği Bölümüen_US
dc.authoridKarakaya, Necati/0000-0002-9447-157X-
dc.authorwosidCelik Karakaya, Muazzez Celik/AAW-6584-2021-
dc.authorwosidKarakaya, Muazzez Celik/ABG-4130-2020-
dc.identifier.volume202en_US
dc.identifier.startpage1en_US
dc.identifier.endpage12en_US
dc.identifier.wosWOS:000465504000001en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.authorscopusid36944318400-
dc.authorscopusid55354186300-
dc.authorscopusid55964403000-
dc.authorscopusid6508252236-
dc.authorscopusid57193777507-
item.fulltextWith Fulltext-
item.grantfulltextembargo_20300101-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.openairetypeArticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
crisitem.author.dept02.07. Department of Geological Engineering-
crisitem.author.dept02.07. Department of Geological Engineering-
crisitem.author.dept07. 04. Department of Chemistry and Chemical Processing Technologies-
crisitem.author.dept02.07. Department of Geological Engineering-
crisitem.author.dept02.07. Department of Geological Engineering-
Appears in Collections:Mühendislik ve Doğa Bilimleri Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collections
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collections
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