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利用１９９２年以来采自南黄海的沉积物样品和１９９６年的南黄海水文调查资料，采用地层对比、沉积动力及环境分析等方法，研究了济州岛西北海域反气旋型涡旋流型的环流性质、其下方泥质沉积物的特征以及它们之间的因果关系，并与南黄海中部的气旋型涡旋沉积进行了深入的对比。结果表明，反气旋和气旋型沉积物都是细粒的泥质沉积，是在沉积动力较弱的低能环境下生成的，但它们之间还存在明显的差异，特别是反气旋型涡旋的沉积厚度大、粒度较粗，进一步反映了两者沉积动力的差别，显示了气旋型涡旋和反气旋型涡旋是具有独立属性的两种低能环境。
Based on the sediment samples collected from the South Yellow Sea since 1992 and the South Yellow Sea hydrologic survey data from 1996, the circulation properties of anticyclone vortex patterns in the northwestern waters of Jeju Island were studied by stratum contrast, sediment dynamics and environmental analysis. , The characteristics of the shale sediments beneath them and the causal relationship between them, and an in-depth comparison with the cyclonic vortex deposition in the central part of the southern Yellow Sea. The results show that both anticyclone and cyclonic sediments are fine-grained muddy sediments, which are formed under low-energy environment with low depositional momentum, but there are still significant differences between them, especially the anti-cyclonic vortex Sedimentary thickness, coarse grain size, further reflecting the difference between the two depositional dynamics, shows that the cyclonic vortex and anti-cyclonic vortex are two independent properties of the low-energy environment.