Tectonics in the northwestern West Philippine basin
文献类型：期刊论文
| 作者 | Ni Xianglong1,3,4; Wu Shiguo1,2; Ryuichi, Shinjo5 |
| 刊名 | JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES
 |
| 出版日期 | 2008-06-01 |
| 卷号 | 19期号:3页码:191-199 |
| 关键词 | Tectonics Amagma Spreading Gravity Anomaly Magnetic Anomaly West Philippine Basin |
| ISSN号 | 1002-0705 |
| 文献子类 | Article |
| 英文摘要 | The West Philippine basin (WPB) is a currently inactive marginal basin belonging to Philippine Sea plate, which has a complex formation history and various crust structures. Based on gravity, magnetic and seismic data, the tectonics in West Philippine basin is characterized by amagma spreading stage and strike slip fractures. NNE trending Okinawa-Luzon fracture zone is a large fracture zone with apparent geomorphology and shows a right-handed movement. The results of joint gravity-magnetic-seismic inversion suggest that the Okinawa-Luzon fracture zone has intensive deformation and is a transform fault. Western existence of the NW trending fractures under Ryukyu Islands Arc is the main cause of the differences between south and north Okinawa Trough. The Urdaneta plateau is not a remained arc, but remnant of mantle plume although its lava chemistry is similar to oceanic island basalt (OIB).; The West Philippine basin (WPB) is a currently inactive marginal basin belonging to Philippine Sea plate, which has a complex formation history and various crust structures. Based on gravity, magnetic and seismic data, the tectonics in West Philippine basin is characterized by amagma spreading stage and strike slip fractures. NNE trending Okinawa-Luzon fracture zone is a large fracture zone with apparent geomorphology and shows a right-handed movement. The results of joint gravity-magnetic-seismic inversion suggest that the Okinawa-Luzon fracture zone has intensive deformation and is a transform fault. Western existence of the NW trending fractures under Ryukyu Islands Arc is the main cause of the differences between south and north Okinawa Trough. The Urdaneta plateau is not a remained arc, but remnant of mantle plume although its lava chemistry is similar to oceanic island basalt (OIB). |
| 学科主题 | Geology ; Geosciences, Multidisciplinary |
| 语种 | 英语 |
| WOS记录号 | WOS:000257294800001 |
| 公开日期 | 2010-12-24 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/5055]  |
| 专题 | 海洋研究所_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 266071, Peoples R China 2.China Univ Petr Huadong, Qingdao 266555, Peoples R China 3.PetroChina, Res Inst Petr Explorat & Dev NW NWGI, Lanzhou 730020, Peoples R China 4.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 5.Univ Ryukyus Senbaru 1 Nishihara, Dept Phys & Earth Sci, Okinawa 9030213, Japan |
| 推荐引用方式 GB/T 7714 | Ni Xianglong,Wu Shiguo,Ryuichi, Shinjo. Tectonics in the northwestern West Philippine basin[J]. JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES,2008,19(3):191-199. |
| APA | Ni Xianglong,Wu Shiguo,&Ryuichi, Shinjo.(2008).Tectonics in the northwestern West Philippine basin.JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES,19(3),191-199. |
| MLA | Ni Xianglong,et al."Tectonics in the northwestern West Philippine basin".JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES 19.3(2008):191-199. |
入库方式： OAI收割
来源：海洋研究所
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