We detected 24 long‐term slow slip events (SSEs) in the western Nankai subduction zone,
Japan, from 1996 to 2017 using a newly developed method: grid‐based determination of …

Low-frequency earthquakes, atypical seismic events distinct from regular earthquakes, occur
downdip of the seismogenic megathrust where an aseismic rheology dominates the …

We determine the first high‐resolution P and S wave attenuation (Q) tomography beneath
the entire Japan Islands using a large number of high‐quality data collected from P and S …

Tremor occurs on megathrusts under conditions of near-lithostatic pore-fluid pressures and
extremely weakened shear strengths. Although metamorphic reactions in the slab liberate …

We use local earthquake velocity spectra to solve for the 3-D distribution of P-and S-wave
attenuation in the shallow Hikurangi subduction zone in the North Island of New Zealand to …

We present a new 3-D anisotropic P-wave velocity (Vp) model for the crust and upper mantle
of the Japan subduction zone obtained by inverting a large number of high-quality P-wave …

We derive an extensive catalog of low‐frequency earthquakes (LFEs) in western and central
Shikoku applying an automatic, coherency‐based detection and location method to 4‐year …

An earthquake swarm in the Wakayama prefecture, Japan, is known as the most active and
persistent swarm, with> 95,000 earthquakes (M≥–1.3) occurring during the 2003–2020 …

Abstract The first three‐dimensional (3‐D) P and S wave attenuation (Qp and Qs)
tomography of the crust and upper mantle of the northern Sumatra subduction zone is …

Slow slip phenomena deep in subduction zones reveal cyclic processes downdip of locked
megathrusts. Here we analyze seismicity within a subducting oceanic slab, spanning~ 50 …