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金牛山金矿床的石英包裹体划分为纯液相包裹体、气液相包裹体和ＣＯ２三相包裹体三种类型，均一温度在１５０～３００℃，主成矿温度在１９０～２１０℃之间。研究表明成矿热液由南向北运移。
Quartz inclusions in Jinniushan gold deposit are divided into three types: pure liquid inclusions, gas-liquid inclusions and CO2 three-phase inclusions. The homogenization temperature is between 150 and 300 ℃ and the main mineralization temperature is between 190 and 210 ℃ . Research shows that hydrothermal fluids migrate from south to north.