东海盆地L凹陷多次波非常发育，严重干扰了地质记录。
Multiple reflection is very developed in L depression of East China Sea, and has severely interfered with normal seismic records.
东海盆地周边地质表明存在有中生代、古生代地层，并有过海相沉积环境。
The geology of the surrounding areas of east China sea basin indicates that Marine environment: existed during middle-late Mesozoic era and late Palaecz - oic era.
本文指出东海盆地是一个大型的以新生代沉积为主的盆地，沉积岩厚度超过万米。
This article indicates that east China sea basin was a large Cenozoic sedimentary basin, with a thickness of deposition of more than 10 thousand meters.
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.
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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