Lithospheric structure of the southeastern margin of the Tibetan Plateau from Rayleigh wave tomography-Reference-Cited by-同舟云学术

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Lithospheric structure of the southeastern margin of the Tibetan Plateau from Rayleigh wave tomography

Published:2017-06 Issue:6 Volume:122 Page:4631-4644
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Fu Yuanyuan V.¹^ORCID,Gao Yuan¹,Li Aibing²^ORCID,Li Lun³^ORCID,Chen Anguo¹

Affiliation:

1. Key Laboratory of Earthquake Prediction; Institute of Earthquake Science, China Earthquake Administration; Beijing China

2. Department of Earth and Atmospheric Sciences; University of Houston; Houston Texas USA

3. ION Geophysical Corporation; Houston Texas USA

Funder

National Natural Science Foundation of China

National Key Research and Development Project of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016JB013096/fullpdf

Reference62 articles.

1. Granite rheology: Magma flow and melt migration;Bagdassarov;J. Geol. Soc.,1998

2. Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging;Bai;Nat. Geosci.,2010

3. Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions;Bao;Earth Planet. Sci. Lett.,2015

4. Himalayan tectonics explained by extrusion of a low-viscosity channel coupled to focused surface denudation;Beaumont;Nature,2001

5. Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen;Beaumont;J. Geophys. Res.,2004

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