An oceanic plateau, the Yakutat terrane, has entered the subduction system across
southcentral Alaska. Its down‐dip fate and relationship to overlying volcanism is still …

NW Canada and Alaska are the continuation of the North American Cordillera through
Mexico, western USA and western Canada. I show that they have similar thermal regimes …

Comprehensive observations of surface wave anisotropy across Alaska and the Aleutian
subduction zone would help to improve understanding of its tectonics, mantle dynamics, and …

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 …

The application of ambient seismic noise cross‐correlation to distributed acoustic sensing
(DAS) data recorded by subsurface fiber‐optic cables has revolutionized our ability to obtain …

While variations in crustal structure beneath the Denali fault in Alaska are well‐documented,
the existence of fault‐correlated structures throughout the entire thickness of the continental …

We perform adjoint waveform tomography to reveal the P‐wave velocity structure of the crust
and uppermost mantle in Alaska by using common‐source double‐difference traveltime …

We obtained a 3D image of crust and mantle seismic velocity gradients beneath the state of
Alaska using common‐conversion point (CCP) stacking of S‐to‐p converted body waves …

I present a 3‐D isotropic shear wave velocity model of the crust and uppermost mantle
beneath the Alaska‐Aleutian subduction zone offshore of the Alaska Peninsula, based on …

Seismic deployments in the Alaska subduction zone provide dense sampling of the seismic
wavefield that constrains thermal structure and subduction geometry. We measure P and S …