Elsewhere, two plates may shift toward each other and converge along a deepsea trench and island arc.
在别的地方，两块板块又可能相向移动而沿着深海沟和岛弧逐渐聚合。
These correlations depend not only on the state of the basic stress field in the island arc-trench but also on the additional stress field caused by the variation of rotation velocity of the earth.
这种特征可能不仅和海洋与大陆板块汇聚边界的岛弧海沟上的基本应力状态有关，而且与自转速率不均匀产生的附加应力状态有关。
Elsewhere, two plates may shift toward each other and converge along a deepsea trench and island arc.
在别的地方，两块板块又可能相向移动而沿著深海沟和岛弧逐渐聚合。
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