...板块构造动力学,地幔对流,俯冲带 [gap=734]Keywords】: China,Geodynamics,Regional stress field,Dynamics of plate tectonies,Mantle convection,Subduction zone ...
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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.
考虑到印度板块的推挤、重力和热应力场的共同作用，可以较好地解释青藏高原构造变形的特点及动力学机制。
Considering stress field caused by combined effect of northward push from Indian plate, gravity and thermal stress, tectonic deformation features in Qinghai Tibet plateau can be understood better.
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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