Among the wide range of thermal, petrologic, hydrological, and structural factors that
potentially affect subduction earthquakes, the roughness of the subducting seafloor is …

Abstract The 2011 March 11 Tohoku-oki great (Mw 9.1) earthquake ruptured the plate
boundary megathrust fault offshore of northern Honshu with estimates of shallow slip of 50 m …

The structure and dynamics in SE Tibet are the key to understand the tectonic evolution of
the Tibetan Plateau. In this study we determined high-resolution P-wave seismic images in …

A high-resolution P-wave tomography of the crust and mantle down to 700km depth beneath
the Japan Islands is determined using a large number of high-quality arrival-time data from …

We determined three‐dimensional P and S wave velocities and P wave azimuthal
anisotropic tomography of the Northwest Pacific subduction zones by inverting 1,225,086 P …

Southeast Asia is surrounded by subduction zones resulting from the interactions of several
lithospheric plates. Its evolution has been also influenced by active tectonics due to the Indo …

A detailed 3‐D model of P wave isotropic velocity and azimuthal anisotropy beneath SE Asia
is obtained by jointly inverting local earthquake arrival times and teleseismic relative travel …

The great 2011 Tohoku‐oki earthquake (Mw 9.0) and its 339 foreshocks and 5,609
aftershocks (9–27 March 2011) were relocated using a three‐dimensional seismic velocity …

The big mantle wedge (BMW) model was originally proposed to explain the origin of the
intraplate Changbaishan volcano in NE China where the subducting Pacific slab becomes …

We determined high-resolution P-wave tomography for 3-D radial and azimuthal anisotropy
of the Tohoku and Kyushu subduction zones using a large number of high-quality arrival …