It used to be considered that the wolframite_quartz veins in Xihuashan orefield has been crystallized from hyperthermal or mesothermal solution. Reported here are fluid-melt inclusions and silicate inclusions within beryl of the wolframite-quartz veins, which coexist with gas-liquid inclusions. This suggests that the metallogenetic fluids should be a kind of magmatic hydrothermal solution. The present paper has probed into the relationship between melt and metallization.