Crustal shear wave velocity and radial anisotropy beneath the Rio Grande rift from ambient noise tomography
Author:
Affiliation:
1. Institute of Earthquake Science, China Earthquake Administration Beijing China
2. Department of GeosciencesUniversity of Houston Houston Texas USA
Funder
NSF
National Natural Science Foundation of China
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014JB011602
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2. Mafic and ultramafic inclusion suites from the Rio Grande rift (New Mexico) and their bearing on the composition and thermal state of the lithosphere
3. A Fast and Reliable Method for Surface Wave Tomography
4. Processing seismic ambient noise data to obtain reliable broad band surface wave dispersion measurements;Bensen G. D.;Geophys. J. Int.,2007
5. A 3-D shear velocity model of the crust and uppermost mantle beneath the United States from ambient seismic noise
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