IOCAS-IR  > 海洋地质与环境重点实验室
Geophysical signature and detection of shallow water flow in the deepwater basin of the northern South China Sea
Wu Shi-Guo1; Sun Yun-Bao1,2; Wang Xiu-Juan1; Zhao Qiang1,2; Liu Feng1,2; Dong Dong-Dong
2010-07-01
发表期刊CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
卷号53期号:7页码:1681-1690
文章类型Article
摘要With the development of deepwater drilling, deepwater geohazards have become a challenge. Shallow water flow (SWF) is one type of the most serious geohazards in deepwater drilling. SWF hazards are only met in deepwater regions and SWF sands have the properties of low density, low velocity and high V(p)/V(s). Based on the theory of Sequence Stratigraphy, the deepwater channel depositional system was identified in Baiyun depression, Pearl River Basin. With the result of AVA inversion, fullwave inversion and poststack inversion, the region with low density, low velocity and high V(P)/V(S)(>9) value were refined in which the SWF may happen.
关键词Shallow Water Flow Deepwater Basin Deepwater Channel System Baiyun Depression
DOI10.3969/j.issn.0001-5733.2010.07.019
收录类别SCI
语种英语
WOS记录号WOS:000280431200019
引用统计
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/32850
专题海洋地质与环境重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
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GB/T 7714
Wu Shi-Guo,Sun Yun-Bao,Wang Xiu-Juan,et al. Geophysical signature and detection of shallow water flow in the deepwater basin of the northern South China Sea[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2010,53(7):1681-1690.
APA Wu Shi-Guo,Sun Yun-Bao,Wang Xiu-Juan,Zhao Qiang,Liu Feng,&Dong Dong-Dong.(2010).Geophysical signature and detection of shallow water flow in the deepwater basin of the northern South China Sea.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,53(7),1681-1690.
MLA Wu Shi-Guo,et al."Geophysical signature and detection of shallow water flow in the deepwater basin of the northern South China Sea".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 53.7(2010):1681-1690.
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