Abstract: In the studied area formations of different structural setting are present. They have been classified and called, inascending order; Davras limestone, Çandır formation, Ophiolitie unit, Sütçüler formation And Aksu Çay formation.Davras limestone is apparently para-autochthonous. Çandır and Sütçüler formations have been correlated with theunits of the Western Taurids, in respect to facies and structure and suggested to be allochthonus,All of the Mesozoic units have been covered by EarlyMiocene Güneyce and Late Miocene Aksu Çay formations.