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以地质和成矿学论点为依据，内岛弧、大陆边缘及内大陆构造域的火山深成岩带的形成作用具有其共同性；矿石－岩浆系可划分数个级别．金－银矿化的矿物－地球化学特点与局部或整体矿石－岩浆系中含矿岩浆岩岩石化学特点之间存在有可比性．通过含矿脉体－交代岩带的形态、构造、结构特点、物质组成变化的研究表明，产出在单独的矿石－岩浆系，特别是高等温线部位的矿床，其垂向成矿规模最大．在地球物理、地质学、岩石学、物理化学和实验研究的基础上建立同火山作用的金－银成矿系模型是可行的
Based on the geological and mineralization arguments, the formation of volcanic and deep-diagenetic zones within the intra-island arc, continental margins and intracontinental tectonics have their commonalities; the ore-magmatism can be divided into several levels. The mineralogical-geochemical features of gold-silver mineralization are comparable with the petrochemical characteristics of ore-bearing magmatic rocks in local or whole ore-magmatic systems. The study on the changes of the ore body, the structure, the structural characteristics and the change of the material composition of the ore belt shows that the vertical mineralization is the largest in the ore-magmatic system, especially in the isothermal ore belt. Based on geophysical, geology, petrology, physicochemical and experimental studies, it is feasible to establish a gold-silver metallogenic model with volcanism