Features of Late Cenozoic Deepwater Sedimentation in Southern Qiongdongnan Basin, Northwestern South China Sea
文献类型：期刊论文
| 作者 | Yuan Shengqiang1,2; Yao Genshun1,2,3; Lue Fuliang3; Hu Bing3; He Xiaosu3; Wang Bin3 ; Li Li3
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| 刊名 | JOURNAL OF EARTH SCIENCE
 |
| 出版日期 | 2009-02-01 |
| 卷号 | 20期号:1页码:172-179 |
| 关键词 | Qiongdongnan Basin Deepwater Sedimentary System Channel Polygon Fault The South China Sea |
| ISSN号 | 1674-487X |
| DOI | 10.1007/s12583-009-0017-0 |
| 文献子类 | Article |
| 英文摘要 | Based on high resolution 2D and 3D seismic data acquired in recent years, using sequence stratigraphy analysis and geophysical methods, we discuss the features of Late Cenozoic deepwater sedimentation in the southern Qiongdongnan (sic) basin. The study area entered a bathyal slope environment in the Miocene. The channel developed in the Sanya (sic) Formation was controlled by a fault break, and its shingled seismic characteristics represent multiple erosion and fill, which may indicate that turbidite current developed in the slope environment. The polygon faults found in mudstone of the Meishan (sic) Formation represent the deepwater hungry sedimentary environment. The large-scale channels developed on the top of Huangliu (sic) Formation could be the result of a big sea level drop and an increase of sediment supply. The fantastic turbidite channel developed in Late Quaternary in the slope environment has "fan-like" body and long frontal tiny avulsion channel. The analysis of these features suggests that the sediment supply of the study area in the post-rifting period was dominant from the Vietnam uplift in the southwest. These deepwater sedimentary features could be potential reservoirs or migration pathways for deepwater petroleum systems.; Based on high resolution 2D and 3D seismic data acquired in recent years, using sequence stratigraphy analysis and geophysical methods, we discuss the features of Late Cenozoic deepwater sedimentation in the southern Qiongdongnan (sic) basin. The study area entered a bathyal slope environment in the Miocene. The channel developed in the Sanya (sic) Formation was controlled by a fault break, and its shingled seismic characteristics represent multiple erosion and fill, which may indicate that turbidite current developed in the slope environment. The polygon faults found in mudstone of the Meishan (sic) Formation represent the deepwater hungry sedimentary environment. The large-scale channels developed on the top of Huangliu (sic) Formation could be the result of a big sea level drop and an increase of sediment supply. The fantastic turbidite channel developed in Late Quaternary in the slope environment has "fan-like" body and long frontal tiny avulsion channel. The analysis of these features suggests that the sediment supply of the study area in the post-rifting period was dominant from the Vietnam uplift in the southwest. These deepwater sedimentary features could be potential reservoirs or migration pathways for deepwater petroleum systems. |
| 学科主题 | Geosciences, Multidisciplinary |
| URL标识 | 查看原文 |
| 语种 | 英语 |
| WOS记录号 | WOS:000264753800017 |
| 公开日期 | 2010-12-22 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/3065]  |
| 专题 | 海洋研究所_实验海洋生物学重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 3.PetroChina Hangzhou Inst Geol, Hangzhou 310023, Zhejiang, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yuan Shengqiang,Yao Genshun,Lue Fuliang,et al. Features of Late Cenozoic Deepwater Sedimentation in Southern Qiongdongnan Basin, Northwestern South China Sea[J]. JOURNAL OF EARTH SCIENCE,2009,20(1):172-179. |
| APA | Yuan Shengqiang.,Yao Genshun.,Lue Fuliang.,Hu Bing.,He Xiaosu.,...&Li Li.(2009).Features of Late Cenozoic Deepwater Sedimentation in Southern Qiongdongnan Basin, Northwestern South China Sea.JOURNAL OF EARTH SCIENCE,20(1),172-179. |
| MLA | Yuan Shengqiang,et al."Features of Late Cenozoic Deepwater Sedimentation in Southern Qiongdongnan Basin, Northwestern South China Sea".JOURNAL OF EARTH SCIENCE 20.1(2009):172-179. |
入库方式： OAI收割
来源：海洋研究所
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