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Active tectonics of the Ortaköy fissure-ridge-type travertines : implications for the Quaternary stress state of the neotectonic structures of the Central Anatolia, Turkey
(supprimer)
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