俯冲带变质脱水作用对俯冲带的流体形成、岩浆起源和演化起着重要的控制作用。
Metamorphic dehydration in subduction zones plays a significant role in the genesis of slab-derived fluids and the generation and evolution of arc magmas.
根据包裹体研究恢复了包裹体形成时期流体的组分、温度和压力。
By studying fluid enclosure, ingredient temperature and pressure is evoluted when fluid enclosure had being formed.
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