Abstract:

Starting around Düzyayla (Sivas) in the north and following Kayseri, Çamardı (Niğde), Kamışlı, Pozantı and Gülek Boğaz, passing from the north of Mersin by approximately K60D direction to Anamur, the Central Anadolu Fay System forms the longest third verified foil generation in Turkey. The remaining part of the Central Anadolu Fay System (CAFS) between Gülek and Anamur is called Namrun Fay Zone. In this study, the geological and morfotectonic properties of Namrun and nearby areas were studied. The foundation of the area located in the southern part of the Central Toros is the Jura - Alt Kretase formation of the Hell, represented by the old Dolomites and Dolomites. This foundation is disconnected by the Santonian-Companyan old Yavca formation, which is composed of square, marn and turbidic square. Both units are covered with a tectonic touch by a mixture of Nuts in Maastricht. These assemblies are overwhelmed by the opposite old rock units. These are, respectively; land-laguner environmental product Oligosen old Gildirli formation; Alt-Miyosen old Kaplankaya formation stored in a thick marine environment and the Alt-Miyosen old Karaisali formation represented with its resifal squares. Namrun Fay Zone is represented in the K60-80D direction and 3-8 km long with a large number of fights in the region. These are, respectively, Namrun, Chamarası, Sebil, Helldere, Alaiye, Tepetaş, Square and Çevlik benefits. The boundaries of the reverse old rock units and the left side deformations observed in the morphology, the foil plate solutions and the earthquakes occurring in the area indicate that these foils are left side-directed foil with an important foil component.