The area under study covers an area in a part of Nort-eastern Taurus Mountains which is a crossing spot between Northern Anatolian Fault Zone and Eastern Anatolian Fault Zone. The rocks here are the products of magmatism starting from the Upper Cretaceous to the Pliocene. Of the series the first from the bottom contains ophiolite and crystallised limestone, and the second from the bottom comprises of plutonic and volcanic rocks with the characters of calcalkaline, acidic, neuter and basic. The magnetite deposists of A-B Kafas of Divriği contains % 55 Fe and possesses roughly 53 million tone visible reserves and possibly 20 million tone hidden reserves in the from of ore vein, stock-work and hollow filling in the felsic roks. The primary minerals' paragenesis of deposits is comprised of both ore minerals namely magnetite, hematite, pyrite, calcopyrite, pyrotine, ilmenite, ilmenomagnetite, rutil-anatas, bravoile, arsenopyrite, sfalarite and native gold, and other minerals whose names are magnetite, scapolite, diopside, biotite, apatite minerals belonging to the mineral paragenesis of deposits are crystallised together (or each other). The existence of trace elements in the bodies of calcopyrite, magnetite and pyrite in high temperature, and of the hematite indicating a speciality of flowing structure under microscope points that all these minerals have been formed from the same magmas and created at the same time. Furthermore, the presence of chlorite, epidote, scopolile, carbonate and quartz minerals, of high proportion of water, and of bearing densely flowing characters shows that it is a spilitic ore magma with alkaline characters. The magma, which is created by the movement of subduction and obduction of plate-tectonic, penetrates into this gabro and converts flowing gases in magma into the felsic roks by influencing the garb in the series of of iyolite.