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Contour-parallel sediment dispersal from the Yangtze Estuary into the East China Sea develops a large-scale mud belt on the inner shelf.
Trapping and escaping processes of Yangtze River-derived sediments to the East China Sea
【摘 要】
：
Contour-parallel sediment dispersal from the Yangtze Estuary into the East China Sea develops a large-scale mud belt on the inner shelf.
【机 构】
：
Centre for Coastal Ocean Science and Technology(CCOST),School of Marine Sciences,Sun Yat-sen Univers
【出 处】
：
海洋湍流混合与沉积物输移过程国际学术研讨会(International Workshop on Turbulent Mi
【发表日期】
：
2016年10期
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