流体包裹体岩相学和显微测温学研究表明，银山矿床石英斑岩和多金属矿脉中都发现有含石盐的高盐度流体包裹体，表明至少在成矿作用的早期成矿流体为高盐度流体。

The fluid-inclusion study at the Yinshan polymetallic ore deposit reports the presence of liquid- and vapor-rich, two-phase inclusions and liquid-rich, high-salinity inclusions containing hilite.

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