Heterogeneity and anisotropy of the lithosphere of SE Tibet from surface wave array tomography
Understanding the geotectonic evolution of the southeastern Tibetan plateau requires knowledge about the structure of the lithosphere. Using data from 77 broadband stations in SW China, we invert Rayleigh wave phase velocity dispersion curves from ambient noise interferometry (T = 10–40 s) and teles...
Main Authors: | Yao, Huajian, Montagner, Jean-Paul, van der Hilst, Robert D |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
Format: | Article |
Language: | en_US |
Published: |
American Geophysical Union
2014
|
Online Access: | http://hdl.handle.net/1721.1/85927 https://orcid.org/0000-0003-1650-6818 |
Similar Items
-
Radial anisotropy in the crust of SE Tibet and SW China from ambient noise interferometry
by: Huang, Hui, et al.
Published: (2012) -
Ambient noise interferometry and surface-wave array tomography in southeastern Tibet
by: Yao, Huajian
Published: (2010) -
Surface-wave eikonal tomography for dense geophysical arrays
by: Gouedard, Pierre, et al.
Published: (2014) -
Crustal radial anisotropy shear wave velocity of SE Tibet from ambient noise tomography
by: Li, Zhengyang, et al.
Published: (2023) -
Surface-wave eikonal tomography in a scattering environment
by: Verdel, Arie, et al.
Published: (2012)