Accurately inferring the radially anisotropic structure of the mantle using seismic waveforms
requires correcting for the effects of crustal structure on waveforms. Recent studies have …

We use normal-mode splitting functions in addition to surface wave phase anomalies, body
wave traveltimes and long-period waveforms to construct a 3-D model of anisotropic shear …

Since the 1960s seismologists have mapped anisotropy in the uppermost mantle, the mantle
transition zone, and the D ″region. When combined with constraints from mineral physics …

A number of recent global tomographic studies have modeled three dimensional variations
in the parameters of radial anisotropy. As yet there is limited agreement among such studies …

We present a tomographic model of radially anisotropic shear velocity variations in the
Earth's mantle based on a new compilation of previously published data sets and a variable …

We investigate whether the coupling of normal mode (NM) multiplets can help us constrain
mantle anisotropy. We first derive explicit expressions of the generalized structure …

Sambridge's Neighborhood Algorithm was applied to normal mode and surface wave phase
velocity data to determine the likelihood of radial anisotropy in mantle reference models …

We present a new global whole‐mantle model of isotropic and radially anisotropic S velocity
structure (SGLOBE‐rani) based on~ 43,000,000 surface wave and~ 420,000 body wave …

A surface wave dispersion data set of unprecedented size is used to obtain a variable‐
resolution model of the radially anisotropic shear wave velocity structure of the upper mantle …

It is well established that the Earth's uppermost mantle is anisotropic, but there are no clear
observations of anisotropy in the deeper parts of the mantle. Surface waves are well suited …