We believe that there were platform sediments in the Paleozoic and the rifting depression sediments from Mesozoic to Cenozoic in the Yellow Sea area.

• 对南、北黄海沉积盆地形成的构造背景和盆地的构造类型进行了研究，认为在古生代它们是台地相沉积，中生代和新生代是张裂盆地；