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Propagators and ridge jumps in a back-arc basin, the West Philippine Basin

文献类型:期刊论文

作者Deschamps, Anne1; Shinjo, Ryuichi2; Matsumoto, Takeshi2; Lee, Chao-Shing3; Lallemand, Serge E.4; Wu, Shiguo5; Sci Party KR03-04 KR04-14 Cruises; Deschamps, A, Univ Brest, CNRS, Univ Europeenne Bretagne,IUEM, UMR Domaines Ocean 6538, Pl N Copern, F-29280 Plouzane, France
刊名TERRA NOVA
出版日期2008-08-01
卷号20期号:4页码:327-332
ISSN号0954-4879
DOI10.1111/j.1365-3121.2008.00824.x
文献子类Article
英文摘要We explore the tectono-magmatic processes in the western West Philippine Basin, Philippine Sea Plate, using bathymetric data acquired in 2003 and 2004. The northwestern part of the basin formed through a series of northwestward propagating rifts. We identify at least five sequences of propagating rifts, probably triggered by mantle flow away from the mantle thermal anomaly that is responsible for the origin of the Benham and Urdenata plateaus. Gravitational forces caused by along-axis topographic gradient and a similar to 30 degrees ridge reorientation appear to also be driving the rift propagations. The along-axis mantle flow appears to be reduced and deflected along the Luzon-Okinawa fracture zone, because the spreading system remained stable west of this major fault zone. North-east of the Benham plateau, a left-lateral fracture zone has turned into a NE-SW-trending spreading axis. As a result, a microplate developed at the triple junction.; We explore the tectono-magmatic processes in the western West Philippine Basin, Philippine Sea Plate, using bathymetric data acquired in 2003 and 2004. The northwestern part of the basin formed through a series of northwestward propagating rifts. We identify at least five sequences of propagating rifts, probably triggered by mantle flow away from the mantle thermal anomaly that is responsible for the origin of the Benham and Urdenata plateaus. Gravitational forces caused by along-axis topographic gradient and a similar to 30 degrees ridge reorientation appear to also be driving the rift propagations. The along-axis mantle flow appears to be reduced and deflected along the Luzon-Okinawa fracture zone, because the spreading system remained stable west of this major fault zone. North-east of the Benham plateau, a left-lateral fracture zone has turned into a NE-SW-trending spreading axis. As a result, a microplate developed at the triple junction.
学科主题Geosciences, Multidisciplinary
URL标识查看原文
语种英语
WOS记录号WOS:000257800500011
公开日期2010-11-18
源URL[http://ir.qdio.ac.cn/handle/337002/1833]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Deschamps, A, Univ Brest, CNRS, Univ Europeenne Bretagne,IUEM, UMR Domaines Ocean 6538, Pl N Copern, F-29280 Plouzane, France
作者单位1.Univ Brest, CNRS, Univ Europeenne Bretagne,IUEM, UMR Domaines Ocean 6538, F-29280 Plouzane, France
2.Univ Ryukyus, Dept Phys & Earth Sci, Okinawa 90302313, Japan
3.Natl Taiwan Ocean Univ, Inst Appl Geophys, Chilung 202, Taiwan
4.Univ Montpellier 2, F-34095 Montpellier 05, France
5.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714
Deschamps, Anne,Shinjo, Ryuichi,Matsumoto, Takeshi,et al. Propagators and ridge jumps in a back-arc basin, the West Philippine Basin[J]. TERRA NOVA,2008,20(4):327-332.
APA Deschamps, Anne.,Shinjo, Ryuichi.,Matsumoto, Takeshi.,Lee, Chao-Shing.,Lallemand, Serge E..,...&Deschamps, A, Univ Brest, CNRS, Univ Europeenne Bretagne,IUEM, UMR Domaines Ocean 6538, Pl N Copern, F-29280 Plouzane, France.(2008).Propagators and ridge jumps in a back-arc basin, the West Philippine Basin.TERRA NOVA,20(4),327-332.
MLA Deschamps, Anne,et al."Propagators and ridge jumps in a back-arc basin, the West Philippine Basin".TERRA NOVA 20.4(2008):327-332.

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来源:海洋研究所

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