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本文根据东海陆架地区新构造运动、地震地质特征以及深部地质特征等,论证了31°30′N,128°00E′的 7242站、水深 155 m附近,现在的水下贝壳沙堤和阶地,就是15,000年前最低海面时期的滨岸产物。
Based on the neotectonic movement, seismic geologic features and deep geological features in the East China Sea shelf area, this paper demonstrates that 7242 stations of 31 ° 30’N and 128 ° 00E ’are near 155 m water depth. Now the underwater shell dike and terraces are The coastal product of the lowest sea level 15,000 years ago.