Middle Miocene mound-shaped sediment packages on the slope of the Xisha carbonate platforms, South China Sea: Combined result of gravity flow and bottom current
文献类型：期刊论文
| 作者 | Wang, Dawei1 ; Zhang, Xinyuan1,3; Wang, Bin4; Ma, Benjun1,3; Lv, Fuliang4; Wu, Shiguo2; Tian, Jie1,3
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| 刊名 | DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
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| 出版日期 | 2015-12-01 |
| 卷号 | 122期号:2015页码:172-184 |
| 关键词 | Mound-shaped Sediment Packages Gravity Flow Bottom Current Xisha Carbonate Platforms South China Sea |
| DOI | 10.1016/j.dsr2.2015.06.016 |
| 文献子类 | Article |
| 英文摘要 | Deep-water mound-shaped sediment packages on the northern slope of the Xisha carbonate platforms in the northern South China Sea were analyzed by integrating high-resolution multi-channel seismic and drilling data. The mounds are distributed in the Beijiao depression of the Qiongdongnan Basin within the T41-T40 seismic horizons, which correspond to the middle Miocene. Mound-shaped reflections were identified both in the NE-SW and NW-SE oriented seismic profiles. The mound shapes are most prominent in the center of the NW-SE oriented seismic profiles, and the undulating tops flatten out towards the NW and SE. Similar reflections are mostly asymmetric, with steeper eastern flanks in the NE-SW oriented seismic profiles, and they are mostly round in shape. The wave impedance from the inversion calculation is 6-8 x 10(6) kg/(m(2).s). It is much lower than that of the reef reservoir in the LH11-1 Reef Oilfield. Paleogeographic analysis shows that the Xisha uplift was dominated by tropical shallow carbonate platforms, while the Beijiao depression became a bathyal environment in the middle Miocene. Drilling data confirmed that the mound-shaped sediment packages are mainly composed of calcareous mudstone. Therefore, we infer that the mound-shaped sediment packages could be reef complexes or they were presumably built by combined gravity flow and bottom current. (C) 2015 Elsevier Ltd. All rights reserved. |
| URL标识 | 查看原文 |
| WOS关键词 | DEEP-WATER CIRCULATION ; PEARL RIVER MOUTH ; QIONGDONGNAN BASIN ; TURBIDITY CURRENTS ; SEISMIC CHARACTERISTICS ; NORTH-ATLANTIC ; SEQUENCE STRATIGRAPHY ; CHANNEL SYSTEM ; NE ATLANTIC ; NEW-ZEALAND |
| 语种 | 英语 |
| 项目编号 | SIDSSE201403 |
| WOS记录号 | WOS:000367106500017 |
| 版本 | 出版稿 |
| 源URL | [http://ir.idsse.ac.cn/handle/183446/1226]  |
| 专题 | 深海科学研究部_深海地球物理与资源研究室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Sanya Inst Deep Sea Sci & Engn, Lab Marine Geophys & Georesource, Sanyo 572000, Peoples R China 3.Univ Chinese Acad Sci, Sch Earth Sci, Being 100049, Peoples R China 4.CNPC, Hangzhou Inst Geol, Hangzhou 310000, Zhejiang, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Dawei,Zhang, Xinyuan,Wang, Bin,et al. Middle Miocene mound-shaped sediment packages on the slope of the Xisha carbonate platforms, South China Sea: Combined result of gravity flow and bottom current[J]. DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY,2015,122(2015):172-184. |
| APA | Wang, Dawei.,Zhang, Xinyuan.,Wang, Bin.,Ma, Benjun.,Lv, Fuliang.,...&Tian, Jie.(2015).Middle Miocene mound-shaped sediment packages on the slope of the Xisha carbonate platforms, South China Sea: Combined result of gravity flow and bottom current.DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY,122(2015),172-184. |
| MLA | Wang, Dawei,et al."Middle Miocene mound-shaped sediment packages on the slope of the Xisha carbonate platforms, South China Sea: Combined result of gravity flow and bottom current".DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY 122.2015(2015):172-184. |
入库方式： OAI收割
来源：深海科学与工程研究所
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