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.
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。
Therefore, they provide important constrains on the tectonic evolution of the NCC and the lithospheric mantle under NCC in this period.
因此，研究其岩石成因和构造背景有助于制约该时期华北克拉通的构造演化过程以及岩石圈地幔的特征和演变规律。
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