中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Tomographic imaging of the Cascadia subduction zone: Constraints on the Juan de Fuca slab

文献类型:期刊论文

作者Chen, Chuanxu1,2,3; Zhao, Dapeng2; Wu, Shiguo4
刊名TECTONOPHYSICS
出版日期2015-04-19
卷号647页码:73-88
关键词Cascadia Juan De Fuca Slab Seismic Tomography Episodic Tremor And Slip Subduction Zone Earthquake
ISSN号0040-1951
DOI10.1016/j.tecto.2015.02.012
文献子类Article
英文摘要We used 40,343 P-wave arrival times from 1883 local earthquakes and 105,455 P-wave arrivals from 6361 teleseismic events to study the detailed structure of the Cascadia subduction zone. We conducted tomographic inversions using a starting velocity model which includes the high-velocity subducting Juan de Fuca slab as a priori information. A number of such slab-constrained inversions are conducted by changing the slab thickness and the velocity contrast between the slab and the surrounding mantle. Our optimal 3-D velocity model fits the data much better than that determined by an inversion with a 1-D homogeneous starting model. Our results show that the subducting Juan de Fuca slab has a thickness of 30-50 km and a P-wave velocity of 1-3% higher than that of the surrounding mantle. Beneath the northern and southern parts of the Cascadia, P-wave velocity is lower in the slab and along the slab interface, which may reflect a more hydrated slab and more active slab dehydration there. The lateral velocity variations may indicate different degrees of slab dehydration and forearc mantle serpentinization. The segmentation in episodic tremor and slip (ETS) is also spatially coincident with the velocity heterogeneities, indicating that the ETS occurrence and recurrence interval are controlled by fluid activity in and around the mantle wedge corner. (C) 2015 Elsevier B.V. All rights reserved.
WOS关键词AMBIENT NOISE TOMOGRAPHY ; SURFACE-WAVE DISPERSION ; FORE-ARC MANTLE ; P-WAVE ; NORTHERN CASCADIA ; SEISMIC EVIDENCE ; OCEANIC-CRUST ; AZIMUTHAL ANISOTROPY ; ELECTRICAL STRUCTURE ; EPISODIC TREMOR
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000353087400006
出版者ELSEVIER SCIENCE BV
资助机构Japan Society for the Promotion of Science(Kiban-S 11050123) ; MEXT(26106005) ; Strategic Priority Research Program of Chinese Academy of Science(XDA11030102) ; National Natural Science Foundation of China(41476046)
源URL[http://ir.qibebt.ac.cn/handle/337004/10429]  
专题中国科学院青岛生物能源与过程研究所
通讯作者Chen, Chuanxu
作者单位1.Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China
2.Tohoku Univ, Dept Geophys, Sendai, Miyagi 9808578, Japan
3.Univ Chinese Acad Sci, Beijing, Peoples R China
4.Chinese Acad Sci, Sanyo Inst Deep Sea Sci & Engn, Sanyo, Peoples R China
推荐引用方式
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Chen, Chuanxu,Zhao, Dapeng,Wu, Shiguo. Tomographic imaging of the Cascadia subduction zone: Constraints on the Juan de Fuca slab[J]. TECTONOPHYSICS,2015,647:73-88.
APA Chen, Chuanxu,Zhao, Dapeng,&Wu, Shiguo.(2015).Tomographic imaging of the Cascadia subduction zone: Constraints on the Juan de Fuca slab.TECTONOPHYSICS,647,73-88.
MLA Chen, Chuanxu,et al."Tomographic imaging of the Cascadia subduction zone: Constraints on the Juan de Fuca slab".TECTONOPHYSICS 647(2015):73-88.

入库方式: OAI收割

来源:青岛生物能源与过程研究所

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