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根据浅地层剖面、海底地貌、柱状样和对钻孔岩心的分析测试数据，论述了南黄海东侧陆架冰消期以来的沉积特征。在冰消期海侵的初期，海水对南黄海东侧陆架早期沉积物的侵蚀和改造形成了滞留砂砾层、席状砂和潮流沙脊。随着海面的上升和海侵范围的扩大，黄海暖流形成并由于它的驱动在南黄海东侧陆架的南部发育涡旋而形成厚层泥质沉积，而在北部（３５°４０至３６°３５Ｎ之间）则形成潮上带－潮坪－浅海沉积序列。中全新世后，强潮流作用在北部陆架形成潮流沙脊；在江华湾形成潮控三角洲。
Based on the data of shallow stratigraphic section, submarine topography, columnar samples and analysis of drilling cores, the sedimentary characteristics of shelf ice on the east side of the South Yellow Sea are discussed. In the initial phase of the ice-sea transgression, the seawater formed the sand-gravel layer, sandy sand and tidal current sand ridge on the early sediments erosion and remodeling on the eastern shelf of the South Yellow Sea. With the rise of the sea surface and the expansion of the transgression, the Huanghai Warm Current formed and was driven to develop thick muddy deposits by vortexing in the southern part of the continental shelf to the east of the southern Yellow Sea, whereas in the north (35 ° 40 ° to 36 ° 35 N) formed tidal zone - tidal flat - shallow sea sedimentary sequence. After the Middle Holocene, the strong tidal current formed a tidal current sand ridge in the northern shelf; the tidal delta formed in the Jiangwan Bay.