中国大陆板内变形普遍比较强烈。
There are widespread and rather strong intraplate deformations in Chinese continent.
岩石属于大陆板内张性构造环境下高侵位形成的壳源重熔型花岗岩类。
The rocks are crustal remelting, shall level granites formed in a within-plate tensional tectonic environment.
携带这些大陆板块的相对运动已经能够被详细地表述出来，但是这些板。
The relative motion of the plates carrying these continents has been.
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