| Subduction of a buoyant plateau at the Manila Trench: Tomographic evidence and geodynamic implications | |
| Fan, Jianke1,2; Zhao, Dapeng3; Dong, Dongdong1,2 | |
| 2016-02-01 | |
| 发表期刊 | GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
 |
| 卷号 | 17期号:2页码:571-586 |
| 文章类型 | Article |
| 摘要 | We determined P-wave tomographic images by inverting a large number of arrival-time data from 2749 local earthquakes and 1462 teleseismic events, which are used to depict the three-dimensional morphology of the subducted Eurasian Plate along the northern segment of the Manila Trench. Dramatic changes in the dip angle of the subducted Eurasian Plate are revealed from the north to the south, being consistent with the partial subduction of a buoyant plateau beneath the Luzon Arc. Slab tears may exist along the edges of the buoyant plateau within the subducted plate induced by the plateau subduction, and the subducted lithosphere may be absent at depths greater than 250 km at approximate to 19 degrees N and approximate to 21 degrees N. The subducted buoyant plateau is possibly oriented toward NW-SE, and the subducted plate at approximate to 21 degrees N is slightly steeper than that at approximate to 19 degrees N. These results may explain why the western and eastern volcanic chains in the Luzon Arc are separated by approximate to 50 km at approximate to 18 degrees N, whereas they converge into a single volcanic chain northward, which may be related to the oblique subduction along the Manila Trench caused by the northwestern movement of the Philippine Sea Plate. A low-velocity zone is revealed at depths of 20-200 km beneath the Manila Accretionary Prism at approximate to 22 degrees N, suggesting that the subduction along the Manila Trench may stop there and the collision develops northward. The Taiwan Orogeny may originate directly from the subduction of the buoyant plateau, because the initial time of the Taiwan Orogeny is coincident with that of the buoyant plateau subduction. |
| 关键词 | Seismic Tomography Manila Trench Subduction Buoyant Plateau Earthquakes |
| DOI | 10.1002/2015GC006201 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000373070100019 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 版本 | 出版稿 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/126250 |
| 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, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 3.Tohoku Univ, Dept Geophys, Sendai, Miyagi 980, Japan |
| 第一作者单位 | 中国科学院海洋研究所 |
| 推荐引用方式 GB/T 7714 | Fan, Jianke,Zhao, Dapeng,Dong, Dongdong. Subduction of a buoyant plateau at the Manila Trench: Tomographic evidence and geodynamic implications[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2016,17(2):571-586. |
| APA | Fan, Jianke,Zhao, Dapeng,&Dong, Dongdong.(2016).Subduction of a buoyant plateau at the Manila Trench: Tomographic evidence and geodynamic implications.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,17(2),571-586. |
| MLA | Fan, Jianke,et al."Subduction of a buoyant plateau at the Manila Trench: Tomographic evidence and geodynamic implications".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 17.2(2016):571-586. |
| 条目包含的文件 | ||||||
| 文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
| Subduction of a buoy（10432KB） | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 | |
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