中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The crust and upper mantle structure beneath Yunnan from joint inversion of receiver functions and Rayleigh wave dispersion data

文献类型:期刊论文

作者Li, Yonghua1; Wu, Qingju1; Zhang, Ruiqing1; Tian, Xiaobo2; Zeng, Rongsheng1
刊名PHYSICS OF THE EARTH AND PLANETARY INTERIORS
出版日期2008-09-01
卷号170期号:1-2页码:134-146
关键词Receiver function Surface wave dispersion Joint inversion Yunnan area
ISSN号0031-9201
DOI10.1016/j.pepi.2008.08.006
文献子类Article
英文摘要In this study, we apply joint inversion of receiver function and Rayleigh wave dispersion (phase and group) velocities data to estimate a shear wave velocity structure for the Yunnan and its adjacent region. Our joint inversion models indicate strong lateral variations in crustal thickness in this area, which increase gradually from 32 km in SE to 56 km in NW of Yunnan. The gradual change in crustal thickness matches with the gradual topography change over this region. Our models also show a uniform crust-upper mantle S-velocity structure across the region, with a 8-22 km thick upper crust (V-s < 3.4-3.5 km/s), overlying a gradational middle-to-lower crust with S-wave velocities up to 3.5-4.1 km/s at Moho depth. The thickness of middle-to-lower crust is correlated with the Moho depth beneath the seismic stations. There exists low-velocity zone in middle-to-lower crust beneath the Yunnan region, especially in the western Yunnan. It is possible that the thick crust in this study area is mainly caused by a more ductile flow in the middle-to-lower crust. The Sn velocities are slightly higher beneath the southern Yangtze block and Southeast Yunnan fold belt (4.35-4.75 km/s) than the other block (4.15-4.35 km/s). This low Sn velocity beneath western Yunnan and Panxi rift may imply that there has been thermal disturbance to the uppermost mantle away from deep structures in this region. The Vs in lower crust and upper mantle are different across the Red-river fault, which imply that Red-river fault is one main boundary fault. Combining results from other geophysical investigations, we conclude that both the Simao terrane and Baoshan-Tengchong terrane tectonically belong to the Gangwana plate. (C) 2008 Elsevier B.V. All rights reserved.
WOS关键词VELOCITY STRUCTURE BENEATH ; SURFACE-WAVE ; COLLISION ZONE ; WESTERN YUNNAN ; CHINA ; PROVINCE ; REGION ; DEFORMATION ; REFRACTION ; AREA
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000260979100013
出版者ELSEVIER SCIENCE BV
资助机构National Science Foundation of China(40574040 ; National Science Foundation of China(40574040 ; Science Foundation for Institute of Geophysics ; Science Foundation for Institute of Geophysics ; Ministry of Science and Technology of China(DQJB06B07) ; Ministry of Science and Technology of China(DQJB06B07) ; 40704011) ; 40704011) ; National Science Foundation of China(40574040 ; National Science Foundation of China(40574040 ; Science Foundation for Institute of Geophysics ; Science Foundation for Institute of Geophysics ; Ministry of Science and Technology of China(DQJB06B07) ; Ministry of Science and Technology of China(DQJB06B07) ; 40704011) ; 40704011) ; National Science Foundation of China(40574040 ; National Science Foundation of China(40574040 ; Science Foundation for Institute of Geophysics ; Science Foundation for Institute of Geophysics ; Ministry of Science and Technology of China(DQJB06B07) ; Ministry of Science and Technology of China(DQJB06B07) ; 40704011) ; 40704011) ; National Science Foundation of China(40574040 ; National Science Foundation of China(40574040 ; Science Foundation for Institute of Geophysics ; Science Foundation for Institute of Geophysics ; Ministry of Science and Technology of China(DQJB06B07) ; Ministry of Science and Technology of China(DQJB06B07) ; 40704011) ; 40704011)
源URL[http://ir.iggcas.ac.cn/handle/132A11/69522]  
专题中国科学院地质与地球物理研究所
通讯作者Li, Yonghua
作者单位1.China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithosphere Evolut, Beijing 100029, Peoples R China
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GB/T 7714
Li, Yonghua,Wu, Qingju,Zhang, Ruiqing,et al. The crust and upper mantle structure beneath Yunnan from joint inversion of receiver functions and Rayleigh wave dispersion data[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS,2008,170(1-2):134-146.
APA Li, Yonghua,Wu, Qingju,Zhang, Ruiqing,Tian, Xiaobo,&Zeng, Rongsheng.(2008).The crust and upper mantle structure beneath Yunnan from joint inversion of receiver functions and Rayleigh wave dispersion data.PHYSICS OF THE EARTH AND PLANETARY INTERIORS,170(1-2),134-146.
MLA Li, Yonghua,et al."The crust and upper mantle structure beneath Yunnan from joint inversion of receiver functions and Rayleigh wave dispersion data".PHYSICS OF THE EARTH AND PLANETARY INTERIORS 170.1-2(2008):134-146.

入库方式: OAI收割

来源:地质与地球物理研究所

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