The basement rocks located in the central part of the southern edge of the Küçük Menderes Graben, around Akçaşehir-Tire are composed of marbles, schists, gneisses and metagabbros of the Ödemiş–Kiraz submassif of the Menderes Massif, and schists, marbles and meta-olistostromes of the Cycladic Complex. | Stratigraphy, sedimentology and palynology of the Neogene–Pleistocene rocks around Akçaşehirtire Izmir (Küçük menderes graben, Western Anatolia)