It is aimed to investigate the ore potential of an area of approximately 132 km2 around Kurşunlu and Dağdere (Selçuklu-Konya). In the study area, Bozdağ formation consisting of recrystallized limestone, dolomitic limestone and dolomites in Silurian (?)-Permian aged Infiltration group belonging to Ladik Metamorphics, Bağrıkurt formation consisting of phyllite, metasandstone, recrystallized limestone, metachert, schist and metacarbonate olistoliths and these units in places. While there are Karadağ metamagmatics that cut into dykes in the intermediate level, in the Ardıçlı group, there are Bahçecik formation represented by metaconglomerate, phyllite metasandstone and recrystallized limestones, and Ertuğrul formation consisting of metacarbonate and metaclastics with gradual transition with this unit. The results of geochemical analysis in the study area showed that there are two main mineralization groups among the ore samples in these units. These are defined as high temperature and low temperature mineralizations. Fe2O3, Cu, Pb, Zn and Mo, which take place in the high temperature mineralization thought to be related to magmatism in the Upper Devonian-Permian period, are quite high in some samples, and Fe2O3 reaches 56.62%, Cu 255 ppm, Pb 685 ppm, Zn. It reaches 1426 ppm and Mo 72 ppm. The second important mineralization is the low-temperature mineralization group, represented primarily by Hg, as well as by Sb, As, Tl, Ag and Au. In some samples, Hg reaches 100 ppm, Sb reaches 182 ppm, As reaches 951 ppm, Tl reaches 20 ppm, Ag reaches 3.3 ppm and Au 63 ppb.