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∼ …

Teleseismic tomography is a powerful tool to study the 3‐D structure of the upper mantle
beneath a local seismic network, but the robustness of its images has been challenged by …

Delamination of the continental lithospheric mantle is well recorded beneath several
continents. However, the fate of the removed continental lithosphere has been rarely noted …

Using recently collected high‐resolution seismic data along a dense linear transect across
Ohio, West Virginia, and Virginia (called Mid‐Atlantic Geophysical Integrative Collaboration …

Continental cratons are characterized by thick lithospheric roots that remain intact for billions
of years. However, some cratonic roots appear to have been thinned or completely removed …

Constraints on the relative contributions of lithospheric and asthenospheric seismic
anisotropy along the eastern passive margin of North America are necessary to further our …