Fault reactivation due to the M 7.6 Nicoya earthquake at the Turrialba‐Irazú volcanic complex, Costa Rica: Effects of dynamic stress triggering

The M 7.6 Nicoya earthquake struck at the interface between the Cocos plate and the Caribbean plate on 5 September 2012 inducing a ground acceleration of 0.5 m s −2 at the Irazú‐Turrialba volcanic complex. We use data from six seismic stations deployed around and atop the Irazú‐Turrialba volcanic complex to show the increase of local seismic activity after the M 7.6 Nicoya earthquake. The response consists in more than 300 locatable earthquakes occurring in swarm sequences along a fault system that intersects the Irazú‐Turrialba volcanic complex. In addition, we point out that major aftershocks are followed by increases of seismic activity in the same region. The weak static stress variation imposed by the main slip of the Nicoya earthquake at the Irazú‐Turrialba volcanic complex suggests a dynamic triggering mechanism. We expand this concept suggesting that this behavior may be similar to the one observed in the Chilean and Japanese volcanic arcs during the M 8.8 2010 Maule, Chile, and M 9.0 2011 Tohoku, Japan, earthquakes. Finally, we highlight that the combined action of dynamic stress and short‐lived coseismic relaxation may trigger seismic activity in geological systems in near‐critical conditions. Distant fault (200 km) reactivated during the M7.6 Nicoya earthquake Threshold of remote triggering for the Nicoya earthquake New mechanism that combines dynamic stress triggering and elastic deformation