A global model of Love and Rayleigh surface wave dispersion and anisotropy, 25–250 s

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An anisotropic shear velocity model of the Earth's mantle using normal modes, body waves, surface waves and long-period waveforms (2014, background): “Several studies have demonstrated that the isotropic shear velocity structure can contain artefacts if anisotropy is not taken into consideration (e.g. Anderson & Dziewoński 1982; Ekström 2011).”
On the limitations of interstation distances in ambient noise tomography (2014, methodology): “Basically, phase velocities are measured by measuring instantaneous phases of each cross-correlation at various periods and unwrapping the instantaneous phases using a global reference phase velocity model GDM52 (Ekström 2011).”