HYDROGEOLOGICAL CHARACTERISTICS OF BEYSEHIR LAKE AND ENVIRONS

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dc.contributor.authorBozdag, Ali
dc.contributor.authorBayram, A. Ferhat
dc.contributor.authorInce, Ismail
dc.date.accessioned2020-03-26T17:27:01Z
dc.date.available2020-03-26T17:27:01Z
dc.date.issued2008
dc.departmentSelçuk Üniversitesien_US
dc.description8th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection -- JUN 16-20, 2008 -- Sofia, BULGARIAen_US
dc.description.abstractThe most important creeks discharging to the Beysehir Lake (Sarisu, Ustunler, Ebulvefa, Eflatun) and their drainage area form the southeast basin of the lake. In this study will be given briefly the rocks in these basins and their hydrochemical relation with surface and subsurface water The Lower - Middle Cambrian Caltepe formation comprises of dolomite, crystallized limestone and nodular limestone, occurs at the basement and, has reservoir rock characteristics. The Upper Cambrian - Lower Ordovician Seydisehir formation overlies conformably the Caltepe formation and comprises of schist, phillite and shale bearing limestone and quartzite lenses in places. The Anamasdagi formation which is the most important reservoir rock in the study area has widespread outcrops around the lake and rest unconformable on the Seydisehir formation. It is composed of conglomerate, marl, sandstone, ferric bauxite, dolomite, limestone and, is Upper Jurassic - Upper Cretaceous in age. The Hoyran complex comprising of serpantinite, pyroxenite, harzburgite, dunite, diabase and chromites emplaced tectonically over the abovementioned units. This unit has outcrops starting from northern part of the Beysehir lake extending approximately in the NNW- SSE direction up to the Yesildag town located at the south of the lake. Besides, the Eocene Buyukkopru formation comes unconformable on these units and, begins at the bottom, with the red marl and continues with mudstone - claystone - turbiditic sandstone. The Toprakli formation is made up of partially consolidated pebble, sand and clay and, covers all the abovementioned units. Karstification and their size in the limestone which are widespread in the basin and which are mostly forming the reservoir rock were interpreted by means of their chemical analysis results. The permeability of alluvial sediments was determined with sieve analysis. The variations in the water level of the lake were interpreted statistically. The chemical analysis results of surface and spring water were evaluated in different diagrams and the possibly of these water as being drinkable and usable were searched.en_US
dc.identifier.endpage706en_US
dc.identifier.isbn978-954-91818-1-4
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage699en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/22446
dc.identifier.wosWOS:000275795400088en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherINT SCIENTIFIC CONFERENCE SGEMen_US
dc.relation.ispartofSGEM 2008: 8TH INTERNATIONAL SCIENTIFIC CONFERENCE, VOL I, CONFERENCE PROCEEDINGS: MODERN MANAGEMENT OF MINE PRODUCING GEOLOGY AND ENVIRONMENTAL PROTECTIONen_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectBeysehir Lakeen_US
dc.subjectHydrogeologicalen_US
dc.subjectCentral Anatoliaen_US
dc.titleHYDROGEOLOGICAL CHARACTERISTICS OF BEYSEHIR LAKE AND ENVIRONSen_US
dc.typeConference Objecten_US

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