h-o isotopes constitute reflects the characteristics of magma flow and metamorphic water interfusion.
石英的氢氧同位素组成反映出巖浆流体与变质水混入溶液特征。
from the isotopic constitutions of hydrogen and oxygen a metamorphic water feature is shown.
氢、氧同位素组成显示变质水特征。
metamorphic water constitutes most of ore-bearing metamorphic hydrothermal water, which tends to mineralize in metamorphic front region and before the front region.
变质水则是含矿变质热液的主体并趋向于在变质前锋区及前锋区前成矿;
the hydrothermal solution mainly came from the metamorphic water mixed witha partial magmatic water.
其中,热液主要来自动热变质水,有部分巖浆热液掺合;