Formed by passive emplacent of crust-mantle mixed type of magma and controlled by nearly NS-trending Baodu-Boluo arcuate fault zone, theHimalayan porphyry belt in Ninglang area tends generally to plunge northward. Porphyry rocks in this belt are intermediate-acid rocks of calc-alkaline series. An integrated analysis of geological and petrochemical characteristics of varus porphyry bodies(groups) in this porphyry belt show that porphyry bodies in this belt are cupreous or copper (molybdenum) ones which have good metallogenic prospects.