GEOLOGICAL, MINERALOGICAL AND GEOCHEMICAL INVESTIGATION OF THE ULUKISLA (NIGDE/TURKEY) EVAPORITES

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dc.authorid0000-0003-1215-8748
dc.contributor.authorTumuklu, Ali
dc.contributor.authorGumus, Hande
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2010
dc.departmentNiğde ÖHÜ
dc.description10th International Multidisciplinary Scientific GeoConference SGEM 2010 -- JUN 20-26, 2010 -- Albena, BULGARIA
dc.description.abstractUlukisla (Nigde/Turkey) evaporites that compose the study area are situated in Ulukisla Basin at the east of Nigde, South of Central Anatolia. The aim of the study is to investigate the geological, mineralogical and geochemical properties of the gypsum and anhydrites in Ulukisla Evaporites and to determine usage area of the evaporites as an industrial material. For this scope, 50 anhydrite and gypsum samples were collected systematically from the Ulukisla evaporites in 900 m thick area. By XRD (X - Ray Diffraction) investigations, the structure of minerals that forms the anhydrites and gypsum, by geochemical analysis major oxides and trace elements percentages, by polarizing microscope, binocular microscope and SEM their mineralogical properties were determined. Result of the geochemical analysis, samples are pure gypsum minerals including some trace elements. Trace elements are Mg, Al, P, K Fe, Rb, and Sr. SEM studies show that there is no different crystal structure in evaporites. Parallel to the surface of lamination and perpendicular to the surface structure was examined. Polarizan microscope studies show the mosaic (lumpy) and diamond mesh textured gypsum. In binocular microscopy examination Selenitic gypsum has transparent structure, and under approximately 1-2 mm thick layer of gypsum, there are needle-like objects can be seen easily. According to the analysis results, gypsum in the region are good quality gypsum for the plaster production.
dc.description.sponsorshipMinist Environm & Water Bulgaria, Bulgarian Acad Sci, Acad Sci Czech Republ, Acad Sci IR Iran, Latvian Acad Sci, Polish Acad Sci, Russian Acad Sci, Serbian Acad Sci & Arts (SASA), Slovak Acad Sci, Natl Acad Sci Ukraine, Bulgarian Ind Assoc
dc.identifier.endpage44
dc.identifier.isbn978-954-91818-1-4
dc.identifier.issn1314-2704
dc.identifier.startpage37
dc.identifier.urihttps://hdl.handle.net/11480/4923
dc.identifier.wosWOS:000288623600006
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.institutionauthor[0-Belirlenecek]
dc.language.isoen
dc.publisherINT SCIENTIFIC CONFERENCE SGEM
dc.relation.ispartof10TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE: SGEM 2010, VOL I
dc.relation.ispartofseriesInternational Multidisciplinary Scientific GeoConference-SGEM
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectGypsum
dc.subjectgeochemistry
dc.subjectUlukisla
dc.subjectTurkey
dc.titleGEOLOGICAL, MINERALOGICAL AND GEOCHEMICAL INVESTIGATION OF THE ULUKISLA (NIGDE/TURKEY) EVAPORITES
dc.typeConference Object

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