矿床类型 该矿床的形成与花岗闪长斑岩具有密切的成因联系，故普遍将该矿床划为斑岩型铜（钼）矿床。但对成矿物质来源的认识，尚不一致。有人强调岩浆-热液体制作用；另一些人则强调围岩体制作用。如杜琦研究认为，多宝山斑岩铜（钼）成矿系统是长期对围岩进行抽吸和有时沿岩浆热液活动中心向上排放的系统。铜质主要来源于围岩，并由围岩提供了大量的水。

The deposit type of the deposit is closely related to the formation of the porphyry copper deposit, so it is generally classified as porphyry copper (molybdenum) deposit. But the source of the ore-forming material is not consistent. It was stressed that the magmatic hydrothermal system, while others stressed the role of the surrounding rock system. Such as Du Qi believes that the metallogenic system of the Duobaoshan porphyry copper (molybdenum) is a long-term of surrounding rock for pumping and sometimes along the magmatic hydrothermal activity center to the exhaust system. The main source of copper in the surrounding rock, and the rock provides a large amount of water.