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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.
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