The pervasive deformation and internal structure of wide continental orogenic belts indicate non-rigid behavior.
大量透入性变形和巨型大陆造山带内部构造显示非刚性特征。
One of them refers to the rotation about vertical axes of crustal blocks in continental areas of diffuse deformation.
第一个是扩散变形的大陆地区其地壳块体绕垂直轴的旋转的问题。
It has not only common characters of continental basins, but also remarkable superimposed fold deformation.
除具陆相盆地的一般特征外，还具有十分突出的叠加褶皱变形特征，因而极为少见。
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