Abstract
Taiwan Shoal sediments are well sorted and rounded medium-coarse sands containing a large amount of shell and beach rock fragments and basalt gravels, and are of deltaic, coastal and colian origin. Underwater sand waves are formed by the combined tidal currents and are remolded by storm waves.
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Aizhi, C., Xiaoning, Z., Yuanmi, L. et al. Sedimentary environment in Taiwan Shoal. Chin. J. Ocean. Limnol. 10, 331–339 (1992). https://doi.org/10.1007/BF02843834
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DOI: https://doi.org/10.1007/BF02843834