Deep earthquakes behave like shallow earthquakes but must have fundamentally different
physical processes. Their rupture behaviors, magnitude-frequency statistics, and aftershocks …

Fluid migration and pore fluid pressure have been implicated in generating the transitional
fault zone properties thought to be important for slow slip events (SSEs) in subduction …

We investigate spatiotemporal changes of intermediate‐depth earthquakes in the double
seismic zone beneath Central and Northeastern Japan before and after the 2011 magnitude …

We investigate the variations of the seismic source properties and aftershock activity using
kinematic inversions and template-matching for six large magnitude intermediate-depth …

Within the last three decades, twelve major earthquakes (Mw> 6.0) have jolted Pakistan and
contributed to a heavy death toll and an economic loss of billions of dollars, which is …

Using seismic data recorded by a dense temporary seismic array, we apply a waveform
matched‐filter technique and obtain an early aftershock catalog around the mainshock …

Intermediate-depth earthquakes occur at temperatures and pressures thought to prohibit
brittle fracture and are deficient in aftershocks compared to shallow earthquakes. We search …

Understanding the interplay of seismic and aseismic slip is key in seismic hazard evaluation.
It is particularly important to know if the same or nearby fault segments can host different slip …

We deployed a seismic network near the source region of the 2017 M w 6.5 Jiuzhaigou
earthquake to monitor aftershock activity and to investigate the local fault structure. An …

Repeating earthquakes provide a novel way of monitoring how stresses load faults between
large earthquakes. To date, however, and despite the availability of long‐duration, high …