陆架海又称“陆棚海”。指占据大陆架的海域。如北海，平均深度96米；楚科奇海，平均深度88米；黄海，平均深度44米；渤海，平均深度21米。
北海、波罗的海以及凯尔特-比斯开大陆架的渔场仍然在走下坡路。
The North Sea, the Baltic and Celtic-Biscay shelf fisheries are all still declining.
大部分的大陆架的活动发生在深水下的大洋洋底的海脊。
Much of the activity between the continental shelves takes place deep underwater at the mid-ocean ridges.
通过分析可以得出如下初步结论：1海槽南部西侧陆架、盆地内部以及琉球岛弧岛坡地震层序是不同的。
According to all of the results, we can concluded that, 1 the seismic sequences developed in the west shelf, trough basin and Ryukyu Island arc are different.
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