Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.13091/5503
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dc.contributor.authorÇelik Karakaya, Muazzezen_US
dc.contributor.authorBozdağ, Aylaen_US
dc.contributor.authorErcan, Hatice Ünalen_US
dc.contributor.authorKarakaya, Necatien_US
dc.contributor.authorDelikan, Arifen_US
dc.date.accessioned2024-05-13T07:11:54Z-
dc.date.available2024-05-13T07:11:54Z-
dc.date.issued2018en_US
dc.identifier.urihttps://hdl.handle.net/20.500.13091/5503-
dc.description.abstractThe study area is located south of the Tuz Gölü Basin in the Central Anatolia. The investigated carbonate minerals are deposited in the Neogene lacustrine sediments. Alternations of halite, carbonate, sulfate minerals and clay-enriched levels have been observed in the ten different drillings made in the study area. The aim of this study is to investigate the properties of carbonate minerals closely related to evaporite minerals, e.g. halite and sulfate minerals. The carbonate minerals commonly observed in the region are dolomite and magnesite which are generally micritic and parallel to bedding and also, they have reticulated structures. The thickness of the carbonate minerals precipitate ranges from mm to dm, and the carbonates have been located as a matrix around other minerals in some levels. The thick carbonate levels indicate to rise of lake level or dilution of the water in the lake. In this study, four carbonate facies have been identified as microbial carbonate facies, sparitic facies, pelloidal facies and oolitic facies. Microbial carbonate facies show quite shallow environments and enriched cyanobacteria. The facies are overlain by generally sparitic cemented peloidal limestones. The Mg/Ca ratio of carbonates is quite high and these high values can be explained by dedolomitization processes. The Sr values of the carbonates range from 115-6216 ppm. The δ18O and δ13C isotope values of the dolomite samples from TG6, TG3 and TG2 drillings range from -3.38 to +5.74 ‰, and -10.78 to +0.04 ‰, respectively. Besides, δ18O and δ13C values of magnesite-rich samples vary between 7.57 and 10.46 ‰ and -4.82 and -9.49 ‰. Isotopic values, sedimentological and geochemical data of carbonates indicate that the deposition environment has sometimes been influenced by atmospheric events, wave activity and water level changes, and also biological activities are highly effective in shapka environment.en_US
dc.language.isoenen_US
dc.publisherAkdeniz Universityen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectTuz Gölüen_US
dc.subjectDolomiteen_US
dc.subjectMagnesiteen_US
dc.subjectδ18Oen_US
dc.subjectδ13Cen_US
dc.titleMineralogical and Stable Isotope Properties of Carbonate Minerals in Tuz Gölü Basin (Turkey): Paleoenvironment Assessmenten_US
dc.typeConference Objecten_US
dc.relation.conference9th International Symposium on Eastern Mediterranean Geology 7-11 May 2018 - Antalya, TURKEYen_US
dc.relation.publication9th International Symposium on Eastern Mediterranean Geologyen_US
dc.relation.isbn978-605-4483-50-1en_US
dc.description.startpage340en_US
dc.description.endpage346en_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeoloji Mühendisliği Bölümüen_US
dc.authorid0000-0003-1104-2110en_US
dc.authorid0000-0002-6114-0678en_US
dc.authorid0000-0002-9447-157xen_US
dc.authorid0000-0003-2895-2954en_US
dc.institutionauthorÇelik Karakaya, Muazzezen_US
dc.institutionauthorBozdağ, Aylaen_US
dc.institutionauthorKarakaya, Necatien_US
dc.institutionauthorDelikan, Arifen_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
item.cerifentitytypePublications-
item.openairetypeConference Object-
item.languageiso639-1en-
item.fulltextWith Fulltext-
item.grantfulltextopen-
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
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