Cycling processes and simultaneous chemical reactions of fluids in subduction zones play an important role in the evolutions of Earth crust and mantle and in the substance exchange.

俯冲带流体循环及伴随的化学作用是壳幔演化和物质交换的重要机制。

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Metamorphic dehydration in subduction zones plays a significant role in the genesis of slab-derived fluids and the generation and evolution of arc magmas.

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。

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