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为了解南海大陆架及邻近海域的基础地质环境，我们于１９９１—１９９５年编制了《南海大陆架及邻近海域基础环境图集》。编图过程中，针对南海的地质地球物理特征，在研究了南海周围地区地质构造及前人研究成果的基础上，提出了南海海盆主要受印澳板块与欧亚板块及太平洋板块与欧亚板块的双重影响。它们之间的相互作用引发南海地区地幔单向流动及流动方向的改变，造成地壳拉张裂陷形成南海海盆的模式
In order to understand the basic geological environment of the South China Sea continental shelf and the adjacent sea areas, we compiled “Atlas of the Basic Environment of the South China Sea Shelf and Adjacent Sea Areas” from 1991 to 1995. In the process of compilation, based on the geological and geophysical characteristics of the South China Sea, based on the study of the geological structure in the area around the South China Sea and the research results of the predecessors, it is proposed that the South China Sea Basin is mainly affected by the Indo-Australian Plate and the Eurasian plate and the Pacific Plate and the Eurasian plate The double impact. The interaction between them leads to the unidirectional flow and the change of the flow direction of the mantle in the South China Sea, resulting in the pattern of the extensional crustal division of the South China Sea Basin