Abstarct: The studied area is located in the Central Iran structural zone and the Sabzevar subzone and at 40 Kilometers to north-northwest of Torbate Heydarieh and through of Kadkan to Robate Sang towns. Copper mineralization at this area occur as stratiform and stratabound within Eocene- Oligocene clastic rock units, with extension at least 65 km. Mineralization in this district is observed discontinuously as Esfiz, Ghandou and Ghonchi deposits and numerous copper indications.......