The rapid expansion of broad-band seismic networks over the last decade has paved the
way for a new generation of global tomographic models. Significantly improved resolution of …

Seismology provides important constraints on the structure and dynamics of the deep
mantle. Computational and methodological advances in the past two decades improved …

We present a new global thermochemical model of the lithosphere and underlying upper
mantle constrained by state of the art seismic waveform inversion, satellite gravity (geoid …

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 …

A large number of fundamental-mode Love and Rayleigh wave dispersion curves were
determined from seismograms for 3330 earthquakes recorded on 258 globally distributed …

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 …

The boundary between the lithosphere and asthenosphere is associated with a platewide
high–seismic velocity “lid” overlying lowered velocities, consistent with thermal models …

A large data set of surface wave phase anomalies, body wave travel times, normal‐mode
splitting functions, and long‐period waveforms is used to investigate the scaling between …

Azimuthal seismic anisotropy, the dependence of seismic wave speeds on propagation
azimuth, is largely due to fabrics within the Earth's crust and mantle, produced by …

According to different types of observations, the nature of lithosphere‐asthenosphere
boundary (LAB) is controversial. Using a massive data set of surface wave dispersions in a …