The fate of water carried by subducted slabs to the deep Earth remains unclear. Experiments suggest that water is unlikely to escape the slabs when they reach the core–mantle boundary despite high pressures and temperatures.

中文翻译：

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深层地幔水更喜欢板块


俯冲板块将水带到地球深处的命运仍不清楚。实验表明，尽管压力和温度很高，但当板块到达核幔边界时，水不太可能从板块中逸出。