The recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

Earthquake prediction remains a challenging and difficult task for scientists all over the
world. The tidal triggering of earthquakes is being proven by an increasing number of …

Low‐frequency earthquakes (LFEs) are small, rapidly recurring slip events that occur on the
deep extensions of some major faults. Their collective activation is often observed as a …

We performed measurements of velocity variations for variable coda waves time lapse using
empirical Green's functions reconstructed by autocorrelation of seismic noise recorded …

Tidal triggering of earthquakes is hypothesized to provide quantitative information regarding
the fault's stress state, poroelastic properties, and may be significant for our understanding of …

Small stress changes such as those from sea level fluctuations can be large enough to
trigger earthquakes. If small and large earthquakes initiate similarly, high‐resolution …

The widespread volcanism on the Jovian moon Io is powered by tidal heating, yet we lack a
deep understanding of how this distinctive heating process affects the locations, timing, or …

Abstract Fracto-emission signals (Acoustic Emission AE, Electromagnetic Emission EME,
and Neutron Emission NE), triggered by high-frequency pressure waves at the different …

Various periodic external loading processes (eg, snow, hydrological and atmospheric, earth
tide and surface reservoir load, etc.) affect tectonic deformation and sometimes modulate …

In many tectonically active regions of the world, a variety of slow deformation phenomena
have been discovered and collectively termed slow earthquakes. Tectonic tremor is the high …