Dongsha erosive channel on northern South China Sea Shelf and its induced Kuroshio South China Sea Branch
文献类型：期刊论文
| 作者 | Luan XiWu1,2; Zhang Liang3,4 ; Peng XueChao5
|
| 刊名 | SCIENCE CHINA-EARTH SCIENCES
 |
| 出版日期 | 2012 |
| 卷号 | 55期号:1页码:149-158 |
| 关键词 | Northern South China Sea margin Dongsha Uplift erosion Dongsha erosive channel Kuroshio South China Sea Branch |
| ISSN号 | 1674-7313 |
| 通讯作者 | Luan, XW (reprint author), Minist Land & Resources, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China. |
| 英文摘要 | Based on a data base of multi-channel seismic profiles covered over Dongsha plateau of the northern South China Sea margin, we found that the sea bed morphology of northern South China Sea margin had been changed dramatically after Dongsha uplifting, that sedimentary layer since Miocene age had been eroded with maximum eroded thickness more than 1000 m, and that an erosive channel had been formed of 20 km in width and 200 km in length and several hundreds meters in depth on the outer shelf of northern South China Sea. The erosive channel is parallel to the 600 m isobath line, stretching from northeast to the southwest north of Dongsha uplift. The Kuroshio intrudes the South China Sea through Luzon Strait both in winter time and summer time, and in the northern South China Sea margin area, the intruded Kuroshio Branch takes the form of Pacific-Indian Ocean Through Flow (PITH) in winter time, while the Luzon Strait Subsurface Inflow (LSSIF) in summer time, the routes of both PITH and LSSIF coincide well with the distribution of the erosive channel. After climbing from the northern slope up to the northern shelf, and after joined by the southward flow from the middle northern shelf of South China Sea, the Kuroshio Branch is strengthened and thus is able to erode the sea floor, and the shape of the erosive channel is a result of the long-term interaction between the Kuroshio South China Sea Branch and the Dongsha outer shelf sea floor. |
| 学科主题 | Geosciences, Multidisciplinary |
| 收录类别 | SCI |
| 原文出处 | 10.1007/s11430-011-4322-y |
| 语种 | 英语 |
| WOS记录号 | WOS:000298967300015 |
| 公开日期 | 2013-09-24 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/12498]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Minist Land & Resources, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China 2.Qingdao Inst Marine Geol, Qingdao 266071, Peoples R China 3.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 4.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 5.Guangzhou Marine Geol Survey, Guangzhou 510760, Guangdong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Luan XiWu,Zhang Liang,Peng XueChao. Dongsha erosive channel on northern South China Sea Shelf and its induced Kuroshio South China Sea Branch[J]. SCIENCE CHINA-EARTH SCIENCES,2012,55(1):149-158. |
| APA | Luan XiWu,Zhang Liang,&Peng XueChao.(2012).Dongsha erosive channel on northern South China Sea Shelf and its induced Kuroshio South China Sea Branch.SCIENCE CHINA-EARTH SCIENCES,55(1),149-158. |
| MLA | Luan XiWu,et al."Dongsha erosive channel on northern South China Sea Shelf and its induced Kuroshio South China Sea Branch".SCIENCE CHINA-EARTH SCIENCES 55.1(2012):149-158. |
入库方式： OAI收割
来源：海洋研究所
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