A 3-D model of the crust and uppermost mantle beneath the Central and Western US by joint inversion of receiver functions and surface wave dispersion-Reference-Cited by-同舟云学术

A 3-D model of the crust and uppermost mantle beneath the Central and Western US by joint inversion of receiver functions and surface wave dispersion

Published:2013-01 Issue:1 Volume:118 Page:262-276
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Shen Weisen¹,Ritzwoller Michael H.¹,Schulte-Pelkum Vera²

Affiliation:

1. Department of Physics; University of Colorado at Boulder; Boulder Colorado USA

2. Cooperative Institute for Research in Environmental Sciences and Department of Geological Sciences; University of Colorado at Boulder; Boulder Colorado USA

Publisher

American Geophysical Union (AGU)

Subject

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

Reference62 articles.

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2. Epicentral location based on Rayleigh wave empirical Green's functions from ambient seismic noise;Barmin;Geophys. J. Int.,2011

3. Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements;Bensen;Geophys. J. Int.,2007

4. Broad-band ambient noise surface wave tomography across the United States;Bensen;J. Geophys. Res.,2008

5. Mapping seismic anisotropy using harmonic decomposition of receiver functions: An application to Northern Apennines, Italy;Bianchi;J. Geophys. Res.,2010

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