特提斯洋关闭和印度板块持续推挤是中国西部前陆盆地形成的构造动力学背景。

Closing of Tethys and continuous compressing and squeezing of Indian plate were the tectonic dynamics background for the formation of foreland basins in western China.

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岩石圈下层的网状塑性流动，作为包含塑性流动网络的黏塑性流动，控制着大陆板块内部的构造变形和动力学过程。

Netlike plastic flow in the lower lithosphere, as viscoplastic flow involving plastic flow network, controls tectonic deformation and dynamic processes within the continental plate.

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指出新的观测资料为板块构造学说和大陆动力学提供了机遇和新的挑战。

In the end new development and challenges on plate tectonics and continent dynamics provided by the new observation are pointed out.

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