中国东部晚第四纪海侵的新构造背景

中国东部沉降海岸及近海钻孔研究表明，第四纪大部分时间里，福建－岭南隆起带基本阻挡了海水大规模进入东海－黄海盆地，约在１６０ｋａ ＢＰ已有低海相性的海侵出现，但是自末次间冰期以来才开始发生大规模海侵，而此时青藏高原正以空前的速率隆升。

THE NEOTECTONIC SETTING OF LATE QUATERNARY TRANSGRESSIONS ON THE EASTERN COASTAL PLAIN OF CHINA

The study of boreholes in the subsided coastal plain and in offshoe area in China shows that at the most part of Quaternary sea water had been blocked from invading the Yellow Sea Basin and Eastern China Sea Basin as a result of the uplifting of Fujian-Lingnan when the Qinghai-Tibetan Plateau was rising at an unprecedented rate.The subsidence of most of Fujian-Lingnan uplift to the sea floor since Late Quaternary had kept the isostatic balance between the Qinghai-Tibetan Plateau and Japan-Ryukyu Island Arc.As sea water entered into the East China Sea and Yellow Sea Basins since about Late Pleistocene, China continent became closely linked to the sea, due to the crustal deformation of the subsidence of continental basins and the corresponding uplifting of the Qinghai-Tibetan Plateau.Since then there has occurred complex land-sea interaction between the Yangtze River, Yellow River, Luanhe River and transgressions caused by the eustatic changes.