结果表明，风暴潮影响后沙滩剖面呈风暴型剖面，而常浪季节均表现为滩肩型复式剖面。
The results showed that the beach profiles belonged to the type of storm profile during storms and of berm profile during other seasons.
这些化石资料表明，宁波组属于一套海陆过渡型沉积，可能为潮间带。
These fossil date indicate that Ningbo Formation is marine-continental transitional sediment, maybe belonging to tidal zone.
沙坝-泻湖型沙滩剖面冲淤变化的主要特征是中潮带形成次一级沙坝。
The main response feature of the bar-lagoon beach profile's was formation of secondary bars at mid tide zone.
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