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斑岩型金矿可分为伴生／共生－斑岩型、角砾／网脉型和单脉／网脉－斑岩型３类。角砾岩筒及其内部构造裂隙、角砾岩筒与围岩的接触带构造、与角砾岩筒有成生关系的断裂构造是斑岩型金矿的重要控矿构造。其由角砾状和网脉状矿石组成，两者又难以划分开，故称角砾／网脉－斑岩型金矿。我国本亚类斑岩型金矿中，往往伴有冰长石化（团结沟、义兴寨、祁雨沟等矿床），个别矿床伴有明矾石化（紫金山矿床），国外同类斑岩型金矿中罕见报道，反映我国此亚类斑岩型金矿的特殊性
Porphyry type gold deposits can be divided into three types: associated / symbiotic-porphyry type, breccia / reticulation type and single vein / reticular-porphyry type. The breccia tube and its internal structural fissures, the contact belt structure between breccia tube and the surrounding rock, and the fault structure which is related to the breccia tube are the important ore-controlling structures of porphyry-type gold deposit. It is composed of brecciated and reticular ores, and they are difficult to separate, so called breccia / veins - porphyry-type gold. In this sub-type of porphyry-type gold deposit in our country, ice feldspar (Tuanjiegou, Yixingzhai and Qiyuogou deposits) are often associated with some Au deposits with alum petrochemical (Zijinshan deposit) Rarely reported in the mines, reflecting the particularity of this sub-type of porphyry-type gold mine in China