Do equilibrium conditions exist during sediment transport studies on continental margins? An example from the East China Sea-Reference-Cited by-同舟云学术

Do equilibrium conditions exist during sediment transport studies on continental margins? An example from the East China Sea

Published:1995-03 Issue:1 Volume:15 Page:23-29
ISSN:0276-0460
Container-title:Geo-Marine Letters
language:en
Short-container-title:Geo-Marine Letters

Author:

Bartek Louis R.,Wellner Robert W.

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Geotechnical Engineering and Engineering Geology,Environmental Science (miscellaneous),Oceanography

Link

http://link.springer.com/content/pdf/10.1007/BF01204494.pdf

Reference22 articles.

1. Alexander CR Jr (1990) Modern sedimentation in the Yellow Sea: Application to geological models of epicontinental-shelf and macro-tidal mudflat environments. Unpublished PhD dissertation. North Carolina State University 198 pp

2. Butenko J, Milliman JD, and Yincan Y (1985) Geomorphology, shallow structure, and geological hazards in the East China Sea. Continental Shelf Research 4:121?141

3. Chang-Shu Y and Jia-Song S (1988) Tidal sand ridges on the East China Sea Shelf. In: de Boer van Gelden A, and Nio SD (Eds.), Tide-Influenced Sedimentary Environments and Facies. Dordrecht: Reidel pp 23?38

4. Choi BH (1980) A tidal model of the Yellow and the Eastern China Sea. Report 80-02. Korean Ocean Research and Development Institute 72 pp

5. Choi BH (1984) Computation of meteorologically-induced circulation in the East China Sea. Marine Geology and Physical Processes of the Yellow Sea 36?48

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