The study area is located in southeast of Qashqasheh Mountain toward northwest of Neyriz. Based on the analyzed samples, the frequency of silica in the samples confirmed the acidic situation of sedimentary environment during the deposition of radiolarite cherts. The radiolarite chert is occurred below the Tarbur Formation and above Bangestan Group. This unit contains Mn minerals. Ore minerals have occurred inside veins, in the groundmass and as a membrane. 9 profiles were studied. The deposit looks like the sedimentary deposit of oceanic basins.