沿消减带的某些板块边界似乎长期无震。
Certain parts of the plate boundaries along subduction zones appear to be aseismic.
与弧背前陆盆地和周缘前陆盆地相并列，并对应于板块构造演化历程中的大洋消减、大陆碰撞和陆内缩短三个不同性质的聚敛阶段。
Therefore they are corresponding to the three different featured convergent stages of ocean subduction, continental collision and intra-continent contraction in the structural evolution of plates.
基底拆离式构造是大陆板块边缘受到俯冲、消减、挤压和缩短作用时，在大陆板块内部的反应。
The basement decoupling structure is the reaction in the continent plate when the marginal of continent plate subducted, subdued, extruding and shorten.
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