Mineralisation associated with fault, vein and shear zone systems can be related to
processes that operated when those systems were active. Despite the complexity of …

In this introduction, we review much of the recent work related to stress transfer, earthquake
triggering, and time‐dependent seismic hazard in order to provide context for the special …

The development of fault interaction models has triggered the need for an accurate
estimation of seismicity rate changes following the occurrence of an earthquake. Several …

We explore the physical conditions that enable triggering of nonvolcanic tremor and
earthquakes by considering local seismic activity on Vancouver Island, British Columbia …

We investigate the triggering of seismic tremor and slow slip event in Guerrero (Mexico) by
the February 27, 2010 Maule earthquake (Mw 8.8). Triggered tremors start with the arrival of …

A fundamental question in earthquake physics is whether aftershocks are predominantly
triggered by static stress changes (permanent stress changes associated with fault …

The paucity of detectable seismicity shadows in the days/months following a main shock has
raised the question as to whether dynamic rather than static triggering could be the main …

In strike-slip fault systems, Coulomb failure stress changes due to mainshocks can trigger
large aftershocks or further earthquakes. The combination of static stress changes from …

Background The occurrence of hydrothermally altered zones is a commonly observed
phenomenon in brittle rock. The dissolution and transformation of primary minerals and the …

The 2004 Aceh and 2005 Nias events are the two greatest earthquakes of the past 40 years
with a total rupture of 1700 km long and a coseismic slip reaching up to 25 m. These two …