Some Geological and Hydrogeochemical Characteristics of Geothermal Fields of Turkey

Basit Öğe Kaydı
dc.contributor.authorSöğüt, Ali Rıza
dc.contributor.authorGüzel, Ahmet
dc.contributor.authorZedef, Veysel
dc.contributor.authorBayram, Ali Ferhat
dc.date.accessioned2020-03-26T18:05:01Z
dc.date.available2020-03-26T18:05:01Z
dc.date.issued2010
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractPresently, active hydrothermal areas of Turkey can be divided into three major provinces which correlate particular volcano-tectonic features. These fields are essentially found at western, central and eastern part of the country. There has been no particular geothermal energy fields in the southern part of Turkey since this region is mostly covered by similar to 2 km thick carbonate sequences and has suffered little recent rifting. The western Turkish geothermal provinces, where horst and graben systems are well developed, have the hottest fluids among others. In this region, normal faults penetrate into the crust and thus the meteoric waters are heated to greater temperatures than in the east where a compressional tectonic regime dominates. In the western Turkish geothermal fields, the fluids have a distinctly higher pH (>7) values than those in the east. This resulted that the Si content of the western Turkish hydrothermal fluids is considerably higher than the others. The geothermal field at Tuzla, situated on the Aegean shore in NW Turkey, has ionic component twice that of conventional seawater. Because of this, the area provides a good opportunity to investigate the interactions between seawater and hot dry rock.en_US
dc.identifier.citationSöğüt, A. R., Güzel, A., Zedef, V., Bayram, A. F., (2010). Some Geological and Hydrogeochemical Characteristics of Geothermal Fields of Turkey. Scientific Research and Essays, 5(20), 3147-3151.
dc.identifier.endpage3151en_US
dc.identifier.issn1992-2248en_US
dc.identifier.issue20en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage3147en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/25272
dc.identifier.volume5en_US
dc.identifier.wosWOS:000284280300014en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.institutionauthorSöğüt, Ali Rıza
dc.institutionauthorGüzel, Ahmet
dc.institutionauthorZedef, Veysel
dc.institutionauthorBayram, Ali Ferhat
dc.language.isoenen_US
dc.publisherACADEMIC JOURNALSen_US
dc.relation.ispartofScientific Research and Essaysen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectGeothermal Fieldsen_US
dc.subjectSeawateren_US
dc.subjectHot Dry Rocken_US
dc.titleSome Geological and Hydrogeochemical Characteristics of Geothermal Fields of Turkeyen_US
dc.typeArticleen_US

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