The investigated area is located at the west of Malatya in Eastern Taurus belt and including an area of approximatelly 200 square kilometers. In this study the subsequent formations have been distinguished from bottom to top: Malatya metamorphics (Permo-Triassic), Berit group (Upper Cretaceous), Polat granitoid (Upper Cretaceous?), Maden complex (Lower-Middle Eocene), Beylerderesi formation (Middle Miocene). The Malatya metamorphics which does not manifest a uniform squence and their consists of various schists, marble, recrystalized limestone and dolomite and their contacts with Polat-Begre granitoid are tectonic and intrusive nature. Berit group are consists of ophiolithic rocks such as dünite, harzburgite amphibolite, gabbro and methapelites. Polat granitoid is represented by plutonic rocks such as diorite, quartz-diorite, tonalite and granodiorite; subvolcanic rocks such as microdiorite, tonalite-diorite porphyrites and dykes such as aplite, andesite and lamprophyre. Maden complex consists of sphilitic basic volcanics, mudstones, micritic limestone, Nummulites-bearing limestone, andesite and diabase dykes and includes some marble blocks. Beylerderesi formation is represented by conglomerate.