通过分析中国大陆地壳运动GPS速度场得到现今构造应变率场。
We obtain contemporary tectonic strain rates of Chinese continent from analyzing crustal motion inferred from GPS velocity field.
这表明，中国大陆地壳现今活动是第四纪以来新构造活动的继续，但也出现了一些新的活动趋势。
It shows that the recent crustal activity in Chinese mainland inherits the neotectonic movement occurred since the Quaternary, while some new activity tendencies appear.
东海陆架盆地是位于中国大陆东部边缘大陆地壳之上的边缘海盆地。
The East China Sea Shelf Basin is a marginal sea basin located on Continental crust of China eastern margin.
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