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。
The pervasive deformation and internal structure of wide continental orogenic belts indicate non-rigid behavior.
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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