中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Deep-Water Bottom Current Research in the Northern South China Sea

文献类型:期刊论文

作者Zheng, HB ; Yan, P
刊名MARINE GEORESOURCES & GEOTECHNOLOGY
出版日期2012
卷号30期号:2页码:122-129
关键词deep-water bottom current Northern South China Sea sediment wave
ISSN号1064-119X
通讯作者hongbozheng@126.com
中文摘要This article discusses an effective way to study deep-water current activity with the sedimentary features of seabed sediments. In the paper, we have processed a seismic survey line crossing the Northwest sub-basin of the South China Sea (SCS). In the seismic profile, we can clearly distinguish the contourite sediment waves and find the erosion scope formed by the deep-water bottom current. Combining the analytic result of piston cores sediments in the research area, we can conclude that the deep-water current is the contour current. It enters the SCS through the narrow Bashi Channel and then it flows to the southwest direction along the isobaths of Dongsha uplift and Southern uplift, but there isn't direct evidence to explain that bottom current flows to the direction of the deep-sea basin. The conclusion confirms former speculation about the passage of deep-water current and provides an important foundation to construct the whole structure of deep-water circulation for the SCS.
学科主题Engineering, Ocean; Engineering, Geological; Oceanography; Mining & Mineral Processing
语种英语
WOS记录号WOS:000303058500002
公开日期2013-08-28
源URL[http://ir.scsio.ac.cn/handle/344004/10361]  
专题南海海洋研究所_中科院边缘海地质重点实验室
推荐引用方式
GB/T 7714
Zheng, HB,Yan, P. Deep-Water Bottom Current Research in the Northern South China Sea[J]. MARINE GEORESOURCES & GEOTECHNOLOGY,2012,30(2):122-129.
APA Zheng, HB,&Yan, P.(2012).Deep-Water Bottom Current Research in the Northern South China Sea.MARINE GEORESOURCES & GEOTECHNOLOGY,30(2),122-129.
MLA Zheng, HB,et al."Deep-Water Bottom Current Research in the Northern South China Sea".MARINE GEORESOURCES & GEOTECHNOLOGY 30.2(2012):122-129.

入库方式: OAI收割

来源:南海海洋研究所

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