New insight into slow earthquake activities from continuous ocean bottom seismometers at the Guerrero seismic gap, Mexico

SUMMARY The Guerrero seismic gap in the Mexican subduction zone exhibits a slip behaviour distinct from that of adjacent segments, which typically experience large earthquakes. With the acquisition of offshore seismic data in this region and the discovery of shallow tectonic tremors, the study of slow earthquakes has gradually increased. This study presents the detection of tectonic tremors and low frequency earthquakes (LFEs) in the Guerrero seismic gap using a combination of a modified envelope cross-correlation method and a matched filter applied to ocean bottom seismometer data for a continuous two-year observational period. The modified envelope cross-correlation method was used to detect and locate tremors, and the matched filter technique enabled the detection of LFEs. These methods allowed for better constraints on the depths of the detected events, offering new insights into tremors and LFE activity offshore the Guerrero seismic gap. Our results show that the spatial distribution of these phenomena, along with seismicity, residual gravity anomalies and seafloor topography, suggests that a section of the shallow plate interface within the gap has experienced stable slip. This study builds on previous work by enhancing the detection and location accuracy of these slow earthquakes, contributing to a more comprehensive understanding of subduction dynamics in the region.