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- W2391471774 abstract "Nanhui eastern mudflat,which has complicated dynamic conditions,sediment transport,sedimentological processes and morphological evolution,is located in the transitional zone between the Yangtze Estuary and the Hangzhou Bay.The comparison of bathymetric charts show that the flat has unitarily extended towards southeast in the past 100 years.The shoreline and flat are dominated by the waves and tide currents and exhibit radial scatter geomorphology and flat slope.As a sub-sand bar,Meimao sand ridge formed in the 1920s had experienced complex geomorphological evolution,but its location and direction of sand ridge remain stable.The stabilization of Meimao sand ridge is sourced from the flat slope of Nanhui eastern mudflat,abundant sediment supplement and proper dynamics of waves and tidal currents." @default.
- W2391471774 created "2016-06-24" @default.
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- W2391471774 date "2007-01-01" @default.
- W2391471774 modified "2023-09-23" @default.
- W2391471774 title "Study on geomorphology evolution of Nanhui eastern mudflat" @default.
- W2391471774 hasPublicationYear "2007" @default.
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