中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The Geometry of the Subducted Slab Beneath Sumatra Revealed by Regional and Teleseismic Traveltime Tomography

文献类型:期刊论文

作者Liu, Shaolin1,2,3,6; Suardi, Iman5; Xu, Xiwei2; Yang, Shuxin2; Tong, Ping1,3,4
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2021
卷号126期号:1页码:29
关键词Seismic tomography Indo‐ Australian plate Sunda plate Sumatra Subduction
ISSN号2169-9313
DOI10.1029/2020JB020169
英文摘要The geometry of the subducted Indo-Australian plate beneath Sumatra is still controversial because of the historical lack of a dense seismic network. Since 2005, Indonesia has been establishing a relatively dense seismic network for real time earthquake monitoring and tsunami warning. The seismic data accumulated by this network make it possible to achieve high-resolution tomographic images of the velocity structure beneath Sumatra by using eikonal equation-based seismic tomography method. Our P-wave tomographic images derived from regional seismic and teleseismic traveltime data demonstrate that the slab in the upper mantle generally follows the strike of the trench and the orientation of the volcanic arc. Additionally, the slab exhibits a sinusoidal shape with a low degree of curvature. Our tomographic results also reveal that the maximum penetration depth of the subducted slab increases from the north to south. The subducted slab beneath the northern tip of Sumatra barely arrives at the 410-km discontinuity, while the slab in the south penetrates to a depth of at least 660 km. Our inversion further indicates that the subducted slab is characterized by a tear at a depth of 120 km between 0 degrees N and 2 degrees N, which may be closely related to the supervolcanic eruption of the Toba caldera in northern Sumatra during the Pleistocene. Moreover, we report that the dip of the subducted slab varies significantly (i.e., dramatically decreases) across the Sunda Strait; therefore, we infer that another subvertical slab tear exists beneath the Sunda Strait.
资助项目National Research Foundation Singapore ; Singapore Ministry of Education under the Research Centers of Excellence Initiative[04MNS001913A620] ; Singapore Ministry of Education under the Research Centers of Excellence Initiative[04MNS001953A620] ; MOE AcRF Tier-1 Grant[04MNP000559C230] ; National Key R&D Program of China[2018YFC1503403] ; National Natural Science Foundation of China[U1839207] ; National Institute of Natural Hazards, Ministry of Emergency Management of China[ZDJ2019-18] ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution[SKL-K201804]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000617378900019
出版者AMER GEOPHYSICAL UNION
资助机构National Research Foundation Singapore ; National Research Foundation Singapore ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; MOE AcRF Tier-1 Grant ; MOE AcRF Tier-1 Grant ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; National Research Foundation Singapore ; National Research Foundation Singapore ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; MOE AcRF Tier-1 Grant ; MOE AcRF Tier-1 Grant ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; National Research Foundation Singapore ; National Research Foundation Singapore ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; MOE AcRF Tier-1 Grant ; MOE AcRF Tier-1 Grant ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; National Research Foundation Singapore ; National Research Foundation Singapore ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; Singapore Ministry of Education under the Research Centers of Excellence Initiative ; MOE AcRF Tier-1 Grant ; MOE AcRF Tier-1 Grant ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; National Institute of Natural Hazards, Ministry of Emergency Management of China ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution ; Open Fund Project of the State Key Laboratory of Lithospheric Evolution
源URL[http://ir.iggcas.ac.cn/handle/132A11/100099]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Tong, Ping
作者单位1.Nanyang Technol Univ, Earth Observ Singapore, 50 Nanyang Ave, Singapore, Singapore
2.Minist Emergency Management China, Natl Inst Nat Hazards, Beijing, Peoples R China
3.Nanyang Technol Univ, Sch Phys & Math Sci, Div Math Sci, Singapore, Singapore
4.Nanyang Technol Univ, Asian Sch Environm, Singapore, Singapore
5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
6.State Key Lab Lithospher Evolut Inst Geol & Geoph, Banten, Indonesia
推荐引用方式
GB/T 7714
Liu, Shaolin,Suardi, Iman,Xu, Xiwei,et al. The Geometry of the Subducted Slab Beneath Sumatra Revealed by Regional and Teleseismic Traveltime Tomography[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2021,126(1):29.
APA Liu, Shaolin,Suardi, Iman,Xu, Xiwei,Yang, Shuxin,&Tong, Ping.(2021).The Geometry of the Subducted Slab Beneath Sumatra Revealed by Regional and Teleseismic Traveltime Tomography.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,126(1),29.
MLA Liu, Shaolin,et al."The Geometry of the Subducted Slab Beneath Sumatra Revealed by Regional and Teleseismic Traveltime Tomography".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 126.1(2021):29.

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来源:地质与地球物理研究所

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