Tidal Coulomb Failure Stresses in the northern Andean intermediate depth seismic clusters: Implications for a possible correlation between tides and seismicity

Abstract

A recent statistical analysis of the relationship between tides and seismic activity in Colombia has suggested the existence of correlation anomalies for the case of intermediate depth events in the Bucaramanga nest and the Cauca cluster (Moncayo et al., 2019). In this work, we explore in detail the hypothesis that tides may be triggering seismic activity in these regions and extend the analysis to two other seismic clusters in northern-central South America, specifically in the areas of El Puyo (Ecuador) and Pucallpa (Peru). For this purpose, we use the available focal mechanism information for seismic events at these locations, and calculate for each event the Tidal Coulomb Failure Stress (TCFS) as obtained from estimations of the tidal strain tensor. Tidal strains are computed considering the Earth body tides and the effect of the ocean tidal loading. Since our purpose is to elucidate the role of tides in earthquake nucleation, calculations of the TCFS are conducted not only for the time of earthquake, but also for the time of the closest maximum strain within a window of a few hours before the events. Our results tend to support the hypothesis that tidal stresses are contributing to earthquake generation in all the studied areas; this trend is especially stronger when TCFS are calculated at pre-earthquake times. The physical explanation for the positive contribution of tides to earthquake triggering in intermediate depth clusters may lie in the fact that a wide diversity of fault plane orientations is possible within a relatively small volume of subducted lithosphere, so making the tides more likely to help loosening up the blocks at the fault plane to promote slip.

Mechanical Mechanism of Fault Dislocation Based on in situ Stress State

“…A critical state of stress is a necessary condition for earthquake occurrence, such as the change of additional normal stress and shear stress caused by tidal action on fault plane (Li and Chen, 2018;Moncayo et al, 2019), which may lead to earthquake; the change of static Coulomb rupture stress caused by earthquake can affect the seismicity nearby (King et al, 1994;Stein, 1999;Wan et al, 2002). Coulomb stress explains the mechanical mechanism of fault dislocation to some extent, but it only pays attention to the stress increment part, ignoring the stress environment of the fault itself (Zhu and Miao, 2016).…”