Modern movement and deformation in the South China Sea shown by GPS measurements and numerical simulation
文献类型：期刊论文
| 作者 | Wang Jing1,2 ; Luan Xiwu3; Yu, Roger Z.4
|
| 刊名 | CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
 |
| 出版日期 | 2013 |
| 卷号 | 31期号:1页码:159-168 |
| 关键词 | stress field deformation mechanical model |
| ISSN号 | 0254-4059 |
| 通讯作者 | Luan, XW |
| 中文摘要 | To better understand the crustal deformation of the South China Sea Basin, we produce a mechanically consistent 2-dimensional model for observing regional velocity field in the South China Sea (SCS). We studied the dominating regional tectonic stress field by geodetic measurements and finite element analysis, the spatial variations of velocity field and strain field, and relative movements among different blocks, using a 2-dimensional model describing crustal deformation of the South China Sea Basin. Strain results show that the SCS is extending at present. The western part of SCS is opening gradually in NWSE direction from its northern margin to the south, but the eastern part of SCS is opening gradually from its central part to the north and south. In addition, we analyzed the plate kinematics to the deformation of the SCS, using a two-dimensional finite element model. Our simulations results are well explained by available geodetic data. The movement of SCS is resulted from interactions among Indian Plate, Pacific Plate, Philippine Sea Plate, and Eurasian Plate. |
| 英文摘要 | To better understand the crustal deformation of the South China Sea Basin, we produce a mechanically consistent 2-dimensional model for observing regional velocity field in the South China Sea (SCS). We studied the dominating regional tectonic stress field by geodetic measurements and finite element analysis, the spatial variations of velocity field and strain field, and relative movements among different blocks, using a 2-dimensional model describing crustal deformation of the South China Sea Basin. Strain results show that the SCS is extending at present. The western part of SCS is opening gradually in NWSE direction from its northern margin to the south, but the eastern part of SCS is opening gradually from its central part to the north and south. In addition, we analyzed the plate kinematics to the deformation of the SCS, using a two-dimensional finite element model. Our simulations results are well explained by available geodetic data. The movement of SCS is resulted from interactions among Indian Plate, Pacific Plate, Philippine Sea Plate, and Eurasian Plate. |
| WOS标题词 | Science & Technology ; Life Sciences & Biomedicine ; Physical Sciences |
| 学科主题 | Marine & Freshwater Biology ; Oceanography |
| 类目[WOS] | Limnology ; Oceanography |
| 研究领域[WOS] | Marine & Freshwater Biology ; Oceanography |
| 关键词[WOS] | RIVER SHEAR ZONE ; CRUSTAL DEFORMATION ; WESTERN PACIFIC ; RED RIVER ; INDO-CHINA ; PHILIPPINES ; ASIA ; LUZON ; EVOLUTION ; MOTION |
| 收录类别 | SCI |
| 原文出处 | 10.1007/s00343-013-2065-7 |
| 语种 | 英语 |
| WOS记录号 | WOS:000313654000018 |
| 公开日期 | 2014-07-17 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/16308]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 海洋研究所_海洋生物技术研发中心 |
| 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 3.China Geol Survey, Inst Marine Geol, Qingdao 266071, Peoples R China 4.Chinese Acad Sci, Inst Oceanol, Editorial Off Chinese Journal Oceanol & Limnol, Qingdao 266071, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang Jing,Luan Xiwu,Yu, Roger Z.. Modern movement and deformation in the South China Sea shown by GPS measurements and numerical simulation[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2013,31(1):159-168. |
| APA | Wang Jing,Luan Xiwu,&Yu, Roger Z..(2013).Modern movement and deformation in the South China Sea shown by GPS measurements and numerical simulation.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,31(1),159-168. |
| MLA | Wang Jing,et al."Modern movement and deformation in the South China Sea shown by GPS measurements and numerical simulation".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 31.1(2013):159-168. |
入库方式： OAI收割
来源：海洋研究所
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