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https://hdl.handle.net/20.500.13091/546
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DC Field | Value | Language |
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dc.contributor.author | Ünal Ercan, Hatice | - |
dc.contributor.author | Çelik Karakaya, Muazzez | - |
dc.contributor.author | Bozdağ, Ayla | - |
dc.contributor.author | Karakaya, Necati | - |
dc.contributor.author | Delikan, Arif | - |
dc.date.accessioned | 2021-12-13T10:26:54Z | - |
dc.date.available | 2021-12-13T10:26:54Z | - |
dc.date.issued | 2019 | - |
dc.identifier.issn | 0883-2927 | - |
dc.identifier.uri | https://doi.org/10.1016/j.apgeochem.2019.04.008 | - |
dc.identifier.uri | https://hdl.handle.net/20.500.13091/546 | - |
dc.description.abstract | The Tuz Golu basin located in Central Anatolia contains ancient (Miocene) and recent evaporite deposits. The aim of this study is to determine the origin and evolution of the ancient halite deposits in the basin, particularly whether there is a marine origin. For this purpose, the mineralogical, geochemical and isotopic properties of halite samples taken from three different drillings at the southern part of the Tuz Golu basin were determined. Halite samples in the Tuz Golu basin are characterized by Cl (60.20-61.00%), Na (39.00-39.40%) and Br (5637 ppm) contents. The Cl-, Br-, Ca, Mg2+, SO42-, and K+ values and Cl/Br (948-86428) ratios indicated that during the formation of the ancient halites in the Tuz Golu basin, the mixture of solutions had different compositions/origins and that the dissolution, recrystallization and dedolomitization mechanisms were effective. The delta Br-81,delta Cl-37, delta Li-7 and delta B-11 isotopic compositions of the pure halites range from - 0.06 to 0.82, - 0.80 to 1.28, - 0.70 to 30.60 and -14.70 to 11.60, respectively. The low delta Cl-37 (from - 0.06 to 0.06 parts per thousand), low delta Br-81 (from 0.03 to 0.95 parts per thousand), high delta B-11 (from -6.40-11.60 parts per thousand) and high delta Li-7 (from 26.00 to 30.60 parts per thousand) values clearly indicate that the brine involved in the formation of the halites of the Tuz Golu basin was largely derived from seawater during the Mid-Miocene Climatic Optimum (MMCO) period. Additionally, the Cl-, Br-, Ca2+, Mg2+, and SO42- contents, as well as the intermediate delta Br-81 (0.34-0.95 parts per thousand) values of the Tuz Golu samples, indicated that the origin of the ancient halites in the basin is not only a marine composition but also a mixture of solutions having different compositions, ratios or origins (e.g., seawater or saline water and groundwater/fresh water). | en_US |
dc.description.sponsorship | Scientific 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.sponsorship | This 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 also thanks to MTA helping us to get the drilling samples. We would like to thank Prof. Dr. Krzysztof Bukowski for their contribution to chemical analyses in AGH laboratories of Poland and we thank the reviewers for their scientific contribution to the paper. | en_US |
dc.language.iso | en | en_US |
dc.publisher | PERGAMON-ELSEVIER SCIENCE LTD | en_US |
dc.relation.ispartof | APPLIED GEOCHEMISTRY | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.subject | Delta Br-81 | en_US |
dc.subject | Delta Cl-37 | en_US |
dc.subject | Delta Li-7 | en_US |
dc.subject | Delta B-11 Isotopes | en_US |
dc.subject | De-Dolomitization | en_US |
dc.subject | Halite | en_US |
dc.subject | Tuz Golu Basin | en_US |
dc.subject | Cl-Br Systematics | en_US |
dc.subject | Fluid Inclusions | en_US |
dc.subject | Central Anatolia | en_US |
dc.subject | Chlorine Isotopes | en_US |
dc.subject | Aqueous-Solutions | en_US |
dc.subject | Early Miocene | en_US |
dc.subject | Pore Waters | en_US |
dc.subject | Sea-Water | en_US |
dc.subject | Bromine | en_US |
dc.subject | Lithium | en_US |
dc.title | Origin and evolution of halite based on stable isotopes (delta Cl-37, delta Br-81, delta B-11 and delta Li-7) and trace elements in Tuz Golu Basin, Turkey | en_US |
dc.type | Article | en_US |
dc.identifier.doi | 10.1016/j.apgeochem.2019.04.008 | - |
dc.identifier.scopus | 2-s2.0-85064456564 | en_US |
dc.department | Fakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeoloji Mühendisliği Bölümü | en_US |
dc.authorid | Karakaya, Necati/0000-0002-9447-157X | - |
dc.authorwosid | Celik Karakaya, Muazzez Celik/AAW-6584-2021 | - |
dc.authorwosid | Karakaya, Muazzez Celik/ABG-4130-2020 | - |
dc.identifier.volume | 105 | en_US |
dc.identifier.startpage | 17 | en_US |
dc.identifier.endpage | 30 | en_US |
dc.identifier.wos | WOS:000468865600003 | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
dc.authorscopusid | 55964403000 | - |
dc.authorscopusid | 36944318400 | - |
dc.authorscopusid | 55354186300 | - |
dc.authorscopusid | 6508252236 | - |
dc.authorscopusid | 57193777507 | - |
dc.identifier.scopusquality | Q2 | - |
item.languageiso639-1 | en | - |
item.fulltext | With Fulltext | - |
item.cerifentitytype | Publications | - |
item.openairetype | Article | - |
item.grantfulltext | embargo_20300101 | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
crisitem.author.dept | 07. 04. Department of Chemistry and Chemical Processing Technologies | - |
crisitem.author.dept | 02.07. Department of Geological Engineering | - |
crisitem.author.dept | 02.07. Department of Geological Engineering | - |
crisitem.author.dept | 02.07. Department of Geological Engineering | - |
crisitem.author.dept | 02.07. 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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