Subducting plates around the globe display a large variability in terms of slab geometry,
including regions where smooth and little variation in subduction parameters is observed …

The pattern of mantle flow in subduction systems and the processes that control the mantle
flow field represent fundamental but still poorly understood aspects of subduction dynamics …

The Pacific Northwest has undergone complex plate reorganization and intense tectono‐
volcanic activity to the east during the Cenozoic (last 65 Ma). Here we show new high …

Using a combination of long period seismic waveforms and SKS splitting measurements, we
have developed a 3-D upper-mantle model (SAWum_NA2) of North America that includes …

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 …

We present high‐resolution 3‐D images of P wave velocity (Vp), azimuthal anisotropy
(AAN), and radial anisotropy (RAN) down to 900‐km depth beneath Alaska obtained by …

The Cascadia margin is an unusual subduction zone characterized by the downdip
movement of young and thin oceanic plates, where mantle flow and intraslab deformation …

The first P-wave tomography of 3-D azimuthal and radial anisotropy of the Cascadia
subduction zone is determined by inverting local and teleseismic arrival-time data. Fast …

In subduction zones with slab‐slab interactions, the pattern of mantle convection is very
complex and still unclear. In this study, we jointly invert a large number of P and S wave …

We present analogue models of free subduction in which we investigate the three-
dimensional (3-D) subduction-induced mantle flow focusing around the slab edges. We use …