现场观测获得了长江口开敞型泥质潮坪不同时间尺度的沉积速率及层偶保存率。
In situ observation has given preservation potentials and deposition rates of non barrier mudflats in the Yangtze River estuary over different time scales.
潮坪观测证明，砂质单层是风暴沉积，而泥质单层是正常天气的沉积单元。
The observation in the Nanhui tidal flat demonstrates that sand layer is deposited by storm, and clay layer is deposited during normal weather.
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