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The radially anisotropic shear velocity structure of the Earth&#39;s mantle provides a critical window on the interior dynamics of the planet, with isotropic variations that are interpreted in terms of thermal and compositional heterogeneity and anisotropy in terms of flow. While significant progress has been made in the more than 30yr since the advent of global seismic tomography, many open question...

Whole-mantle radially anisotropic shear velocity structure from spectral-element waveform tomography