Low wave speed zones in the crust beneath SE Tibet revealed by ambient noise adjoint tomography-Reference-Cited by-同舟云学术

Low wave speed zones in the crust beneath SE Tibet revealed by ambient noise adjoint tomography

Published:2014-01-22 Issue:2 Volume:41 Page:334-340
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Chen Min¹²,Huang Hui¹,Yao Huajian¹³,van der Hilst Rob¹,Niu Fenglin²⁴

Affiliation:

1. Department of Earth and Planetary Sciences; Massachusetts Institute of Technology; Cambridge Massachusetts USA

2. Department of Earth Science; Rice University; Houston Texas USA

3. Laboratory of Seismology and Physics of Earth's Interior; School of Earth and Space Sciences; University of Science and Technology of China; Hefei Anhui China

4. State Key Laboratory of Petroleum Resource and Prospecting, and Unconventional Natural Gas Institute; China University of Petroleum; Beijing China

Funder

XSEDE

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference26 articles.

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2. Partial melt in the upper-middle crust of the northwest Himalaya revealed by Rayleigh wave dispersion;Caldwell;Tectonophysics,2009

3. Topographic ooze: Building the eastern margin of Tibet by lower crustal flow;Clark;Geology,2000

4. Kinematics and dynamics of the southeastern margin of the Tibetan Plateau;Copley;Geophys. J. Int.,2008

5. Radial anisotropy in the crust of SE Tibet and SW China from ambient noise interferometry;Huang;Geophys. Res. Lett.,2010

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