中国大陆东、南边缘经历了欧亚板块与太平洋板块和特提斯板块会聚作用的复杂过程。
Southeastern China continental margin has undergone a complicated convergence process of the Eurasian plate with the Pacific plate and Tethys plate.
也可能加勒比板块将会聚集成一团并整体移动。
Presumably, also, the Caribbean Plate would hold together and move as one.
利用现代空间大地测量技术测出北半球活动板块边缘会聚、扩张和滑动速度。
The convergent and divergent velocities of active plate boundaries in the north hemisphere are obtained with space geodetic data.
图5。菲律宾造山带（孵化的黑色边框与交叉）环绕菲律宾海（注）-巽他（苏）会聚板块边界（重色线）。
Figure 5. The Philippines orogen (black outline with cross-hatching) surrounds the Philippine Sea (PS) - Sunda (SU) convergent plate boundary (heavy colored lines).
准噶尔盆地南缘的晚新生代构造变形被认为是天山地区对印度和欧亚板块的碰撞与会聚作用过程的构造响应。
The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.
准噶尔盆地南缘的晚新生代构造变形被认为是天山地区对印度和欧亚板块的碰撞与会聚作用过程的构造响应。
The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.
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