Pleistocene forced regressions and tidal sand ridges in the East China Sea

Author:

Berné Serge,Vagner Pierre,Guichard François,Lericolais Gilles,Liu Zhenxia,Trentesaux Alain,Yin Ping,Yi Hi Il

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference58 articles.

1. Aloı̈si, J.C., 1986. Sur un modèle de sédimentation deltaı̈que: contribution à la connaissance des marges passives. Unpubl. Ph.D. Thesis, University of Perpignan, 162 pp.

2. Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge;Bard;Nature,1996

3. Do equilibrium conditions exist during sediment transport studies on continental margins? An example from the East China Sea;Bartek;Geo-Mar. Lett.,1995

4. Belderson, R.H., 1986. Offshore tidal and non-tidal sand ridges and sheets: Differences in morphology and hydrodynamic setting. In: Knight, R.J., McLean, J.R. (Eds.), Shelf Sands and Sandstones. Canadian Society of Petroleum Geologists, Calgary, pp. 293–301.

5. Berné, S., Durand, J., Weber, O., 1991. Architecture of modern tidal dunes (sand waves), Bay of Bourgneuf, France. In: Miall, A.D., Tyler, N. (Eds.), Three Dimensional Facies Architecture of Terrigenous Clastic Sediments and its Implications for Hydrocarbon Discovery and Recovery. Concepts in Sedimentology and Paleontology. SEPM, Tulsa, OK, pp. 245–260.

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