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PORTAIL D'INFORMATION GÉOGRAPHIQUE

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  • Several geothermal fields are located in a NE-SW trend along a structural lineament around the Sivas basin. By evaluating the rocks of the Late Miocene-Early Pliocene Kızılırmak Formation, it was determined that fissure axes developed within Ortaköy
  • a result of NW-SE-directed compression, which was also responsible for the formation of the Sivas Backthrust. Ground-penetrating radar studies have shown that the thickness of fissure fills within the fissure-ridge-type travertines of the Ortaköy geothermal