Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

Tsunamis are unpredictable and infrequent but potentially large impact natural disasters. To
prepare, mitigate and prevent losses from tsunamis, probabilistic hazard and risk analysis …

Abstract National Research Institute for Earth Science and Disaster Resilience (NIED)
integrated the land observation networks established since the 1995 Kobe earthquake with …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

Most destructive tsunamis are caused by seismic slip on the shallow part of offshore
megathrusts. The likelihood of this behaviour is partly determined by the interseismic slip …

Continuously operating global positioning system sites in the North Island of New Zealand
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …

Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …

Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

Slow slip events have become recognized in the last decade as an important mode of fault
slip, and are most widely observed at subduction zones. Many episodes of tectonic tremor …

Episodic tremor and slow slip (ETS) occurs in the transition zone between the locked
seismogenic zone and the deeper, stably sliding zone. Actual mechanisms of ETS are …