这些特征表明早石炭世激流河花岗岩类中的暗色包体是岩浆混合的产物，部分代表了混合岩浆的基性端元。
These features indicate that dark inclusions in the Early Carboniferous Jiliuhe granites are the product of magma mixing and partly represent the basic end-member of mixed magma .
激流河