因为大陆壳日益增长，所以了解俯冲带是非常重要的。
It is important to understand subduction because this is where the continental crust grew progressively with time.
对于榴辉岩俯冲折返过程中的壳-幔相互作用及地球化学循环是中国大陆科学钻探工程（CCSD）研究的重点之一。
One main target of the CCSD project is to reveal the mantle-crust interaction and geochemical recycling during continental subduction and eclogite exhumation.
扬子大陆与秦岭造山带之间的壳内构造边界不具陆内俯冲性质，而是逆冲推复一走滑构造带。
The tectonic boundary between the Yangtze Continent and Qinling orogenic belt is a thrust-strike slip tectonic zone rather than a intracontinental subduction zone.
UHPM记录了显生宙俯冲-碰撞造山带早期碰撞过程中的低热流梯度及陆壳的深俯冲作用。
HPM-UHPM registers the low thermal gradients and deep subduction of continental crust during the early stage of the collision process in Phanerozoic subduction-to-collision orogens.
这证明了在大陆地壳岩石俯冲的过程中，石榴石作为水的载体是可以将水携带到地幔深处。
This indicates that garnet, as a carrier of fluids, is able to bring water into the mantle while continental rocks were subducted.
这证明了在大陆地壳岩石俯冲的过程中，石榴石作为水的载体是可以将水携带到地幔深处。
This indicates that garnet, as a carrier of fluids, is able to bring water into the mantle while continental rocks were subducted.
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