This experimental conclusion is of great significance to understanding of the continental magma origins and the deep crust compositions.
这一实验结果对大陆地区岩浆起源和深部地壳物质组成的研究可能有新的启示。
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.
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。
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