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《Journal of Tongji University(Natural Science)》 1979-02
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Preliminary Study on Sedimentary Facies and Sequence of the Yangtze Delta

Li Cong Xian Wan Jing Tai Li Ping  
The Yangtze delta, a large complicated delta system, has an area of about 51800 km2, of which the subaqueous area amounts to 29000 km~2. The delta is fed by Yangtze River which extents inland for more than 6300 km and has an annual sediment discharge of 486 million tons. At the mouth of the river, the average tide range is 2.25 m. and the tide currents play an importent role in delta formation. Combined analyses of 700 submarine surface samples and more than 500 cores have led to the follow conclusions: 1. Yangtze delta consists of the delta proper, and associated depositional systems which include large sand bar in Chien-Tang Estuary, offshore tidel radiate sand bars near Jiang-Gang, and strand plain along both southern and northern flanks of delta. 2. In terms of hydrodanamical setting, sedimental characteristics and palaeomicrofauna assemblage, the delta can be classified into delta plain facies, delta front facies and prodelta facies, and each of which may further be divided into subfacies. About 11 distinct subfacies are presented in Yangtze delta system (see fiqure 7). 3. The deltaic facies sequence observed in descending order from the numerous cores at the river mouth bars and on delta plain correspond well with lateral occurrance of deltaic depositional facies from land toward sea.
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