Investigation of the geothermal system in region of Selime (Turkey) by resistivity methods

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dc.authoridOZTURK, ERNAM/0000-0002-4007-6638
dc.authoridIrmak, Tahir Serkan/0000-0002-4504-6286
dc.authoridHoskan, Nihan/0000-0001-5507-9818;
dc.contributor.authorYeken, Tekin
dc.contributor.authorHoskan, Nihan
dc.contributor.authorOzturk, Ernam
dc.contributor.authorIrmak, Tahir Serkan
dc.date.accessioned2025-10-11T20:47:58Z
dc.date.available2025-10-11T20:47:58Z
dc.date.issued2025
dc.departmentDüzce Üniversitesien_US
dc.description.abstractThe Anatolian platform continues its development with highly complex tectonic activities in Central Anatolia, known as tectonic deformation. In addition to faulting due to the plate movements, the fluid dynamics in the underground and the thermal cycle are also affected. Heater mass circulation plays a role in the development of plate tectonics. This study was aimed to determine the geothermal potential of Selime (Aksaray) and its surroundings. The resistivity method was applied in field studies for the objectives. Geothermal fields with high thermal potential have been investigated by Vertical Electric Sounding (VES) profiles. In the field study, five vertical electric soundings (VES) were applied, a general resistance of (50 - 60) S2m was observed, and Selim tuff was determined at a depth of approximately (30-35) m. A sudden resistance drop of (1-2) S2m under the Selime tuff layer proved the existence of a geothermal source. When examined with the hydrogeological data, a thermal fluid is present with an impermeable cover layer. As a result of this research, it was observed that the heater mass affected the thermal fluid, indicating that circulation represented a shallow system.en_US
dc.identifier.doi10.22201/igeof.2954436xe.2025.64.1.1738
dc.identifier.endpage1415en_US
dc.identifier.issn0016-7169
dc.identifier.issn2954-436X
dc.identifier.issue1en_US
dc.identifier.scopus2-s2.0-85214005970en_US
dc.identifier.scopusqualityQ4en_US
dc.identifier.startpage1395en_US
dc.identifier.urihttps://doi.org/10.22201/igeof.2954436xe.2025.64.1.1738
dc.identifier.urihttps://hdl.handle.net/20.500.12684/21650
dc.identifier.volume64en_US
dc.identifier.wosWOS:001382557600003en_US
dc.identifier.wosqualityQ4en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherInst Geophysics Unamen_US
dc.relation.ispartofGeofisica Internacionalen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.snmzKA_WOS_20250911
dc.subjectSelimeen_US
dc.subjectresistivityen_US
dc.subjectgeothermal fluiden_US
dc.subjectheater mass convectionen_US
dc.titleInvestigation of the geothermal system in region of Selime (Turkey) by resistivity methodsen_US
dc.typeArticleen_US

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