岸线的后退使得M2、S2分潮无潮点位置也不断向西南方向移动。
Tide counting positions of the M2, S2 partial tide move unceasingly to southwest direction following the coastline recession.
东达村组自下而上为冲积扇泥石流沉积、无障壁碎屑滨岸沉积和浅水碳酸盐台地潮坪沉积。
The Dongdacun Formation consists in ascending order of alluvial fan debris flow deposits, barrier-free clastic littoral deposits and shallow-water carbonate platform tidal-flat deposits.
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