Size distribution of detrital mineral grains suspended in surface waters of the Yellow Sea and East China sea

Author:

Yamamoto Satoshi

Publisher

Springer Science and Business Media LLC

Subject

Oceanography,General Earth and Planetary Sciences,Earth-Surface Processes,General Engineering,Soil Science,General Environmental Science

Reference25 articles.

1. Bond, G. C. andR. H. Meade (1966): Size distribution of mineral grains suspended in Chesapeake Bay and nearby coastal waters. Chesapeake Sci.,7, 208–212.

2. Emery, K. O. (1955): Grain size of marine beach gravels. J. Geol.,63, 39–50.

3. Emery, K. O., Y. Hayashi, T. W. C. Hilde, K. Kobayashi, J. H. Koo, C. Y. Meng, H. Niino, J. H. Osterhagen, L. M. Reynold, J. M. Wageman, C. S. Wang andS. J. Yang (1969): Geological structure and some water characteristics of the East China Sea and the Yellow Sea. United Nations ECAFE, CCOP Tech. Bull.,2, 3–43.

4. Emery, K. O., F. Lepple, L. Toner, E. Uchupi, R. H. Rioux, W. Pople andE. M. Hulburt (1974): Suspended matter and other properties of surface waters of the northeastern Atlantic Ocean. J. Sed. Pet.,44, 1087–1110.

5. Emery, K. O. andJ. D. Milliman (1978): Suspended matter in surface waters: Influence of river discharge and of upwelling. Sedimentology,25, 125–140.

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