The charac teristics of homogenization temperature and salinity data also reports that this high - salinity inclusions were not generated by aqueous fluid immiscibility or boiling in ore - forming processes , but generated directly from a water - saturated crystallizing magmatic melt and that the main mechanism of ore deposition is the mixing of magmatic fluid and underwater not boiling of hydrothermal solution 均一温度和盐度特征还表明，高盐度包裹体不是由热水溶液的不混溶作用或沸腾作用形成的，而是由岩浆熔体直接分离的卤水形成的；沸腾作用对矿质沉淀的作用不大，而流体的混合作用是银山矿床矿质沉淀的主要机制。
