Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic
radiation patterns that differ from those of traditional earthquakes. However, slow …

Despite decades of observational, laboratory and theoretical studies, the processes leading
to large earthquake generation remain enigmatic. However, recent observations provide …

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 …

The scaling law for slow earthquakes, which is a linear relationship between seismic
moment and duration, was proposed 15 y ago and initiated a debate on the difference in …

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 …

This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …

Geodesy, the oldest science, has become an important discipline in the geosciences, in
large part by enhancing Global Positioning System (GPS) capabilities over the last 35 years …

The discovery of slow-slip phenomena has revolutionized our understanding of how faults
accommodate relative plate motions. Faults were previously thought to relieve stress either …

Earthquakes occur mainly on active faults. Fault slip is closely related to seismicity and is
thus widely discussed in Geosciences, Seismology, and Engineering. Slip experiment is a …