Oceanic lithosphere moves over a mechanically weak layer (asthenosphere) characterized
by low seismic velocity and high attenuation. Near mid-ocean ridges, partial melting can …

We develop a 3‐D isotropic shear velocity model for the Alaska subduction zone using data
from seafloor and land‐based seismographs to investigate along‐strike variations in …

Anelastic attenuation provides key insight in our understanding of thermal and rheological
structures and the associated deformation and dynamic mechanisms of the Earth's deep …

The Seoul metropolitan area, the most densely populated part of the Korean Peninsula,
features complex subsurface structures and seismogenic faults, though their characteristics …

This study presents the velocity structures of the seafloor sediment across the Pacific using
teleseismic body waves recorded by arrays of ocean bottom seismometers (OBSs). We …

To clarify the internal structure of the oceanic lithosphere-asthenosphere system, here we
determine a new 3-D model of azimuthal anisotropic shear-wave velocity (Vs) down to∼ …