A Fast and Reliable Method for Surface Wave Tomography

By M. P. Barmin, M. Ritzwoller, A. Levshin. 2001

157 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/3d0a5653ea5351b61af834eaa8f98b3ead82bf44

Citations in the corpus

• Ambient noise Rayleigh wave tomography across Europe (2007, unknown): “T O M O G R A P H Y The dispersion measurements of Rayleigh waves from 1 yr crosscorrelations are used to invert for group velocity maps on a 1◦ × 1◦ grid across Europe using the ray theoretic tomographic method of Barmin et al. (2001).”
• Helmholtz surface wave tomography for isotropic and azimuthally anisotropic structure (2011, unknown): “In contrast with traditional tomographic methods (e.g. Trampert & Woodhouse 1996; Ekstrom et al. 1997; Barmin et al. 2001), the inverse operator of eikonal tomography is simply the spatial gradient applied to the phase traveltime map, which is a purely local operator that does not depend on…”
• On the limitations of interstation distances in ambient noise tomography (2014, unknown): “We perform tomography for both data sets using a tomography method of Barmin et al. (2001).”
• 3‐D surface wave tomography of the Piton de la Fournaise volcano using seismic noise correlations (2007, unknown): “[ 9 ] We perform a tomographic inversion of the arrival-time measurements deduced from the group velocity measurements at each period using the algorithm described by [ Barmin et al. , 2001].”
• Eikonal tomography: surface wave tomography by phase front tracking across a regional broad‐band seismic array (2009, unknown): “(b) Same as (a), but the straight-ray inversion of Barmin et al. (2001) is used.”
• Broadband ambient noise surface wave tomography across the United States (2008, unknown): “In later sections, we discuss howmeasurements from almost 20,000 inter-station paths are selected to be used for tomographic inversion to estimate group and phase speed dispersion maps [Barmin et al., 2001] ranging from 8 to 70 s period for Rayleigh waves and 8 to 25 s period for Love waves.”
• A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion (2016, unknown): “apply the traditional ray theoretic method of Barmin et al. (2001) to all ambient noise”
• Thermodynamic constraints on seismic inversions (2004, unknown): “The first step is surface wave tomography (e.g. Barmin et al. 2001; Ritzwoller et al. 2002) in which the measured dispersion curves are inverted to produce 2-”