Ambient noise tomography with a large seismic array

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A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion (2016, methodology): “Earthquake data are processed via eikonal tomography (Lin et al. 2009) in Northeast China or Helmholtz (Lin & Ritzwoller 2011b) tomography in South China, which differ based on whether a finite frequency correction is applied (e.g. Ritzwoller et al. 2011).”
Helmholtz surface wave tomography for isotropic and azimuthally anisotropic structure (2011, methodology): “This justifies the use of eikonal tomography at short periods (<50 s) to constrain shallow structures in the crust and uppermost mantle, particularly when the amplitude information is not available such as for ambient noise application (e.g. Lin et al. 2011; Ritzwoller et al. 2011).”