The East China Sea Shelf Basin is a marginal sea basin located on Continental crust of China eastern margin.
东海陆架盆地是位于中国大陆东部边缘大陆地壳之上的边缘海盆地。
The earth′s crust of the South China Sea belongs to the transitional type between the oceanic crust and continental crust.
南海地壳属于大洋型地壳与大陆型地壳之间的过度类型。
It is China's special continental crust that decides the unique of petroleum in China.
中国陆壳的特殊性，决定了中国石油的特殊性。
The South China Sea is a huge marginal sea at East-Asian continental margin, and a tectonic region of the transitional crust type from continental to oceanic.
南海是东亚大陆边缘的巨型陆缘海，属大陆—大洋过渡型地壳构造区。
The existence of NW-SE direction mantle flow under the continental crust in the north continental margin of South China Sea made the extension activities migrate from north to south.
南海北部陆缘下NW-SE方向流动的地幔流的存在使得伸展活动具有由北向南发育的机制。
The existence of NW-SE direction mantle flow under the continental crust in the north continental margin of South China Sea made the extension activities migrate from north to south.
南海北部陆缘下NW-SE方向流动的地幔流的存在使得伸展活动具有由北向南发育的机制。
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