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云南宁蒗地区喜山期斑岩带各斑岩体（群）地质特征、岩石地球化学等方面的研究表明，斑岩属含矿斑岩。斑岩体侵位的围岩各地层亦具一定的含矿性。随着斑岩带围岩含矿层位和斑岩岩浆含矿性的变化，斑岩型铜矿和斑岩体外接触带矿床也随之发生变化，形成由一系列多矿种、多类型矿床构成的矿床系列。宁蒗地区喜山期斑岩带及其成矿系列严格受ＳＮ向的包都—波罗弧形断裂带控制，该斑岩带实为构造、斑岩、成矿三位一体的喜山期构造—斑岩成矿带。
Geological characteristics and lithochemistry of each porphyry (group) of the Himalayan porphyry belt in Ninglang area, Yunnan Province indicate that porphyries are porphyry-bearing porphyries. The porphyry body emplacement of the surrounding rock is also a certain ore-bearing. With the variation of the ore-bearing beds and the porphyry magma in the porphyry belt, the deposits of porphyry-type copper deposits and in-vitro contact belt of porphyry also change, forming a series of multi-mineral and multi-type deposits Constitute a series of deposits. The Xishan porphyry belt and its metallogenic series in Ninglang area are strictly controlled by the SN direction of the Baodu-Polo arc fault zone. The porphyry belt is really the structure of the Himalayan structure- Porphyry metallogenic belt.