“…The recent evolution of the northern Aegean is characterized by the westward motion of the Anatolian plate along the North Anatolian Fault (e.g. Jolivet, 2011) which in turn pushes the Aegean plate southwards (Papazachos, Kiratzi, & Kontopoulou, 1998;Pavlides et al, 2010). The main active tectonic structures in the study area can be found in the Greek Database of Seismogenic Sources -GreDaSS which done by a group of researchers (Caputo, Chatzipetros, Pavlides, & Sboras, 2013).…”