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。
The tectonic evolution of South China Sea is very complicated because it is located in the convergent hinge of European-Asia plate, Pacific plate and India-Australia -plate.
南海处于欧亚板块、太平洋板块和印度-澳大利亚板块的交汇处，演化历史复杂。
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