Abstract: Starting From the geological background of mineralization, deposit geological characters, ect., the ore-controlling factors of the deposit are analyzed. It is concluded that this deposit is controlled by the stratum lithology, structure and magmatic rock, and that medium acidic porphyry rockmass, skarnization, and gossan are the ore-prospecting indicators. It is preliminarily considered that the depth of this deposit, the east Shizidao region, the heave area at the south syncline axial part are the important orientation in the future ore-prospecting.

Key words: Copper deposit, Ore-controlling factors, Ore-prospecting orientation