大陆岩石圈地幔的古老形成年龄与上覆地壳克拉通的古老稳定年龄相耦合。
The ancient formation age of continental lithospheric mantle is coupling with the age of overlying craton crust.
这是全球首例由橄榄岩-熔体相互反应造成的岩石圈地幔大规模的组成变化。
This is the first case in the world for large-scale compositional changes of the lithospheric mantle resulting from peridotite-melt interaction.
这一研究为了解华南内部中新生代以来陆下岩石圈地幔的属性以及构造演化提供了重要的信息。
This study will provide important information for well understanding and probing into the nature and tectonic evolution of sub-continental lithospheric mantle since the Mesozoic-Cenozoic.
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