Mantle fluids were mostly derived from dehydration and degassing of a subducting slab, mantle original residual volatiles and partial melting of the mantle.

 
  • 俯沖板塊的脫水脫氣作用、地幔原始殘留揮發(fā)份及地幔部分熔融作用是地幔流體的主要來(lái)源。
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