Physical modeling of lithospheric plate deformation is a powerful tool in the reconstruction of plate tectonic evolution.
岩石圈板块变形物理模拟是对板块构造演化的近似再现，代表了板块构造研究的一种主要方向。
Such structure in the collision foredeep of the Dabieshan Orogen was resulted in inelastic extensional deformation of the conver side of the flexed plate aroused by lithospheric flexure.
这些伸展构造很显然是扬子克拉通和华北克拉通在三叠纪碰撞时，大别山造山带前陆位置岩石圈弯曲导致地壳上部产生非弹性变形的结果。
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