The development of Central Anatolian Cenozoic basins such as Sivas, Çankırı, and Tuz Gölü was related to a series of geological processes that occurred after the closure of the northern branch of the Neo-Tethyan Ocean (Şengör and Yılmaz, 1981;Dirik et al., 1999) (Figure 1). An assemblage of ophiolite mélange related to the İzmir-Ankara-Erzincan suture zone crops widely out in eastern and northeastern parts of the basin (Tatar, 1982;Cater et al., 1991). The Sivas Cenozoic Basin is located on three crucial continental plates. These are the Central Anatolian massif in the west, Pontide Thrust Belt in the north, and Tauride-Anatolian Block in the south. On the other hand, older geological units are exposed in the southern part of the basin. They belong to the suture zone of the Inner Tauride Ocean, which was opening and closing between the Jurassic and the Cretaceous/Paleocene periods (Oktay, 1982;Görür et al., 1984;Tekeli et al., 1992). Since the geological structure of the Sivas Basin is so interesting, many researchers have carried out multidisciplinary studies on the basin (