“…This deformation pattern is seen obviously in Kuşadası and Söke areas located at the westernmost tip of the Büyük Menderes Graben (Gürer et al, 2001), in the Halitpaşa graben (Kaya et al, 2004), along the northern margin of the Kiraz half graben located at the eastern tip of the Küçük Menderes graben (Bozkurt & Rojay, 2005), in the Künüpe section of the Büyük Menderes detachment fault zone, to the northeast of Kızıldere settlement located north-eastern margin of the Büyük Menderes Graben (Şimşek, 1985), around Acıdere village located on the southern slope of the Çökelezdağ which comprises the Çivril Graben (Koçyiğit, 2013b), in the apex of Isparta Angle (Boray, Saroğlu, & Emre, 1985), in the Deresenek section of the Akşehir-Afyon Graben (Koçyiğit, Ünay, & Saraç, 2000) and in the Yenigediz-Erdoğmuş Graben (Kütahya) (Gürboğa, Koçyiğit, & Ruffet, 2013). In addition, older graben fill is always folded in not only the Gediz and Büyük Menderes grabens shaped by the detachment normal fault zone, but also in and outside the whole of rest grabens, which lack detachment fault zones but included in the south-western Turkey neotectonic domain (Bozkuş, 1996;İnci, 1991Koçyiğit, 1983Koçyiğit, , 1997Koçyiğit & Deveci, 2007;Koçyiğit, Gürboğa, & Kalafat, 2013;Koçyiğit, Gürboğa, & Ruffet, 2013;Yağmurlu, 1991).…”