PRELIMINARY MINERALOGICAL AND CHEMICAL PROPERTIES OF HALITE IN THE SOUTH OF TUZGOLU BASIN (TURKEY)

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dc.contributor.authorErcan, Hatice
dc.contributor.authorKarakaya, Muazzez Celik
dc.contributor.authorKarakaya, Necati
dc.contributor.authorBozdag, Ayla
dc.contributor.authorDelikan, Arif
dc.date.accessioned2020-03-26T19:42:22Z
dc.date.available2020-03-26T19:42:22Z
dc.date.issued2017
dc.departmentSelçuk Üniversitesien_US
dc.description3rd International Scientific Conference on Geobalcanica -- MAY 20-21, 2017 -- Skopje, MACEDONIAen_US
dc.description.abstractThe study area is located in the southern parts of Tuzgolu basin namely closed Konya basin, which is one of the largest inner/closed basin of Neogene age in the Central Anatolia (Turkey). The basin was mostly filled with the Late Cretaceous-Quaternary aged different types of minerals. The basin, in deep, starts red colored clastic sediments which are formed from thick red clastic unit was deposited in shallow-deep-shallow marine environments. This study was primarily focused on the textural properties of halite mineral in the Miocene units. The textural properties of the halite mineral have been investigated mainly for detection of environmental conditions and origin of halites as primary and secondary halites. Remnant of chevrons structures are most common primary texture preserved in ancient halite deposits. Upward-growing chevrons determined in the halite minerals show that these textures contain rich fluid inclusions and have cloudy or milky appearance. Halite minerals are interlayered with carbonate, sulfate and clay minerals in the studied core samples. The halite layers are generally observed in thick of mm-dm, salt deposits in the dm-m in size precipitated when condition are suitable that huge thickness of shoal water evaporite can accumulate in very short time frames. The thin laminates of halite indicate the fluid chemistry causing the precipitation and changed in a short time interval of the environment condition. The presence of hoper-textures in halite minerals indicated that the first precipitated on the shallow hyper saline brine pools and when they were undisturbed by wind and waves. The secondary marks were commonly observed in the drillings as the nodular structure anhydrite and mosaic texture of halite. The ratios of Cl/Br and Na/Br in the studied halite samples have very high values that are in relation to dissolution and mixing.en_US
dc.description.sponsorshipScientific and Technological Research Council of TurkeyTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [TUBITAK 114Y629]; Selcuk University Scientific Research ProjectsSelcuk University [16401034]en_US
dc.description.sponsorshipThe project was funded by The Scientific and Technological Research Council of Turkey (TUBITAK 114Y629) and the Selcuk University Scientific Research Projects (16401034) support program.en_US
dc.identifier.doi10.18509/GBP.2017.04en_US
dc.identifier.endpage29en_US
dc.identifier.startpage23en_US
dc.identifier.urihttps://dx.doi.org/10.18509/GBP.2017.04
dc.identifier.urihttps://hdl.handle.net/20.500.12395/35396
dc.identifier.wosWOS:000466905500004en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.language.isoenen_US
dc.publisherGEOBALCANICA SOCen_US
dc.relation.ispartof3RD INTERNATIONAL SCIENTIFIC CONFERENCE GEOBALCANICA 2017en_US
dc.relation.ispartofseriesInternational Scientific Conference Geobalcanica Proceedings
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectHaliteen_US
dc.subjectTuzgoluen_US
dc.subjecthopper textureen_US
dc.subjectevaporationen_US
dc.subjectCl/Br ratioen_US
dc.titlePRELIMINARY MINERALOGICAL AND CHEMICAL PROPERTIES OF HALITE IN THE SOUTH OF TUZGOLU BASIN (TURKEY)en_US
dc.typeConference Objecten_US

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