We determine high‐resolution tomographic models of isotropic P‐wave velocity (Vp) and
tilting‐axis anisotropy of the Alaska subduction zone using a large number of local and …

SUMMARY The Alaska–Aleutian subduction zone represents an ideal location to study
dynamics within a mantle wedge. The subduction system spans several thousand …

We estimate depth‐dependent azimuthal anisotropy and shear wave velocity structure
beneath the Alaska subduction zone by the inversion of a new Rayleigh wave dispersion …

Increasing evidence from seismic methods shows that anisotropy within subduction zones
should consist of multiple layers. To test this, we calculate and model shear wave splitting …

The complex tectonic setting of south-central Alaska is characterized by a transition from
normally-dip** subduction of the Pacific plate in the west to near-flat slab subduction of …

Shear wave splitting (SWS) is regarded as the most effective geophysical method to
delineate mantle flow fields by detecting seismic azimuthal anisotropy in the earth's upper …

Abstract The Eastern Gulf of Corinth (EGoC) is one of the most seismically active areas in
Greece. It is monitored by local and regional seismic stations of the Hellenic Unified Seismic …

Shear‐wave splitting observations can provide insight into mantle flow, due to the link
between the deformation of mantle rocks and their direction‐dependent seismic wave …

To investigate the effects of a slab edge and varying slab geometry on the mantle flow
systems beneath south central Alaska, a total of 971 pairs of teleseismic shear wave (SKS …

Seismic anisotropy can provide valuable constraints for the study of subduction zone
dynamics. This study presents a high‐resolution 3‐D azimuthally anisotropic shear wave …