The Baiyun Slide Complex, South China Sea: A modern example of slope instability controlling submarine-channel incision on continental slopes
文献类型：期刊论文
| 作者 | Li, Wei3,4; Alves, Tiago M.; Rebesco, Michele1; Sun, Jie3; Li, Jian4; Li, Shuang4; Wu, Shiguo6 |
| 刊名 | MARINE AND PETROLEUM GEOLOGY
 |
| 出版日期 | 2020 |
| 卷号 | 114页码:UNSP 104231 |
| 关键词 | South China Sea Submarine landslide Submarine channels Bottom currents Turbidity currents |
| ISSN号 | 1873-4073 |
| DOI | 10.1016/j.marpetgeo.2020.104231 |
| 英文摘要 | The Baiyun Slide Complex is one of the largest submarine landslides on the northern margin of the South China Sea. Newly acquired high-resolution bathymetric data, 2D and 3D seismic data permitted the systematic investigation of the Baiyun Slide Complex in terms of its seafloor morphology and associated sedimentary processes. The headwall region of the Baiyun Slide Complex, located at a water depth between 1000 m and 1700 m, is U-shaped and opens towards the east. It was efficiently and almost completely evacuated, generating pronounced headwall and sidewall scarps. Submarine channels, sediment waves, migrating channels, sediment drifts and moats are observed within and around the headwall region, illustrating the effects of both downslope and along-slope sedimentary processes. Submarine channels are 1637 km-long 800-1500 m-wide, and 20 to 50 m-deep. As a modern example of the interplay between slope instability and subsequent incision, submarine channels were generated after the formation of the Baiyun Slide scar to suggest intensified downslope sedimentary processes after the slope collapsed. The initiation and formation of these submarine channels result from the evacuation of the Baiyun Slide scar, which provided the necessary space of the continental slope to accommodate subsequent turbidity and mass wasting flows. Our results are an important example of how submarine landslides can influence erosional and depositional processes on continental margins. |
| 源URL | [http://ir.scsio.ac.cn/handle/344004/18556]  |
| 专题 | 南海海洋研究所_中科院边缘海地质重点实验室 |
| 作者单位 | 1.Alves, Tiago M.] Cardiff Univ, Sch Earth & Ocean Sci, 3D Seism Lab, Main Bldg,Pk Pl, Cardiff CF10 3AT, Wales 2.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanyo 572000, Peoples R China 3.Chinese Acad Sci, South China Sea Inst Oceanol, CAS Key Lab Ocean & Marginal Sea Geol, Guangzhou 510301, Peoples R China 4.Chinese Acad Sci, Innovat Acad South China Sea Ecol & Environm Engn, Guangzhou 510301, Peoples R China 5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 6.Ist Natl Oceanog & Geofis Sperimentale OGS, Borgo Grotto Gigante 42-C, I-34010 Trieste, Italy |
| 推荐引用方式 GB/T 7714 | Li, Wei,Alves, Tiago M.,Rebesco, Michele,et al. The Baiyun Slide Complex, South China Sea: A modern example of slope instability controlling submarine-channel incision on continental slopes[J]. MARINE AND PETROLEUM GEOLOGY,2020,114:UNSP 104231. |
| APA | Li, Wei.,Alves, Tiago M..,Rebesco, Michele.,Sun, Jie.,Li, Jian.,...&Wu, Shiguo.(2020).The Baiyun Slide Complex, South China Sea: A modern example of slope instability controlling submarine-channel incision on continental slopes.MARINE AND PETROLEUM GEOLOGY,114,UNSP 104231. |
| MLA | Li, Wei,et al."The Baiyun Slide Complex, South China Sea: A modern example of slope instability controlling submarine-channel incision on continental slopes".MARINE AND PETROLEUM GEOLOGY 114(2020):UNSP 104231. |
入库方式： OAI收割
来源：南海海洋研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。