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Western Anatolia in Turkey is one of the areas in which the earth`s continental crust has been rapidly deformed. The dominant system is a graben system in western part of the Anatolia. There are various suggestions about the type of the deformation, the amount of extension and the formation of grabens. The regional tectonic structures of western Anatolia is characterized by strike-slip and normal fault zones. Tuzla fault zone, in Izmir in Western Anatolia, is one of the most important of them. The seismic activity...