The Role of Bottom Currents on the Morphological Development Around a Drowned Carbonate Platform, NW South China Sea-Reference-Cited by-同舟云学术

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The Role of Bottom Currents on the Morphological Development Around a Drowned Carbonate Platform, NW South China Sea

Published:2022-07-19 Issue:4 Volume:21 Page:801-812
ISSN:1672-5182
Container-title:Journal of Ocean University of China
language:en
Short-container-title:J. Ocean Univ. China

Author:

Yu Kaiqi,Alves Tiago M.,Li Wei,Li Shuang,Li Jian,Zhao Fang,Wu Shiguo,Zhan Wenhuan

Publisher

Springer Science and Business Media LLC

Subject

Ocean Engineering,Oceanography

Link

https://link.springer.com/content/pdf/10.1007/s11802-022-5020-4.pdf

Reference69 articles.

1. Alves, T. M., 2010. A 3-D morphometric analysis of erosional features in a contourite drift from offshore SE Brazil. Geophysical Journal International, 183: 1151–1164.

2. Andresen, K. J., Huuse, M., and Clausen, O. R., 2008. Morphology and distribution of Oligocene and Miocene pockmarks in the Danish North Sea-Implications for bottom current activity and fluid migration. Basin Research, 20: 445–466.

3. Bertoni, C., Kirkham, C., Cartwright, J., Hodgson, N., and Rodriguez, K., 2017. Seismic indicators of focused fluid flow and cross-evaporitic seepages in the eastern Mediterranean. Marine and Petroleum Geology, 88: 472–488.

4. Betzler, C., and Eberli, G. P., 2019. Miocene start of modern carbonate platforms. Geology, 47: 771–775.

5. Betzler, C., Brachert, T. C., and Kroon, D., 1995. Role of climate in partial drowning of the Queensland Plateau carbonate platform (northeastern Australia). Marine Geology, 123: 11–32.

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