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25 April 2024
 
  » arxiv » 1812.1104

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Tidal Coulomb Failure Stresses in the Northern Andean intermediate depth seismic clusters and its implications for a possible correlation between tides and seismicity
Gloria A. Moncayo ; Gaspar Monsalve ; Jorge I. Zuluaga ;
Date 26 Nov 2018
AbstractA recent statistical analysis of the relationship between tides and seismic activity in Colombia has suggested the existence of correlation anomalies for the case intermediate depth events in the Bucaramanga nest and the Cauca cluster (Moncayo et al., 2018). 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 the northern part of South America, specifically in the areas of Puyo (Ecuador) and Pucallpa (Peru). For this purpose, we use the available focal mechanism information for almost hundred events in the area, 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 both, the Earth Body Tides (BT) and the effect of the Ocean Tidal Loading (OTL). Since our purpose is to elucidate the role of tides in earthquake nucleation, calculations of the TCFS are made 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. Additional tests on the earthquakes within the Bucaramanga nest indicate that the monthly phase is the main tidal contributor to the earthquake generation process. Our results are in agreement with the suggestion that in the zones of seismic clusters, and given their intermediate depth conditions where compressional stresses are expected (Turcotte and Schubert, 2002), the lunisolar forces may contribute to facilitate the displacement of blocks, and hence the triggering of seismic activity.
Source arXiv, 1812.1104
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