作者依据获得的直接证据 (首次发现的含矿喷气岩等 )和间接证据 (组构标型、矿物标型及同位素标型等 ) ,并应用活动论的观点确认天宝山岩块、早二叠世庙岭组、红叶桥组是主要的含矿层 ,每一岩浆单元晚期的中小斑岩是含矿岩。其中的成矿物质在火山喷气、岩浆爆破和断裂构造的热动力驱动下活化并参与成矿 ,这样就使富含成矿物质层 (岩 )真正变成矿源。 Based on the direct evidence (the first discovered ore-bearing jet rock, etc.) and the indirect evidence (texture type, mineral type and isotopic pattern), the authors confirm that the Tianbaoshan block and the Early Permian The Shi Miaoling Formation and the Hongyeqiao Formation are the main ore-bearing formations. The late small porphyry of each magmatic unit is an ore-bearing rock. The metallogenic materials, activated by the thermodynamic power of volcanic jet, magmatic blasting and fault tectonics, are involved in metallogenesis, thus making the ore-rich material layer (rock) truly become a mineral source.