Proceedings of the 12th International INQUA meeting on paleoseismology, active tectonic and archaeoseismology

Fig. 1: a) The map shows the location of the study area, highlighting the Puerto Aldea Fault as the focal point of the study. The GOY seismic stations correspond to the temporary network used for this postdoctoral project, while station CO06 is part of the primary network of the National Seismological Center (CSN). The slab depth in the study area is based on Hayes et al. (2012). Geological, geomorphological, and structural information is modified from Saillard et al. (2009, 2012) and Emparán and Pineda (2006). b) The seismic profile (PBT01) shown at the bottom corresponds to one of the thirty profiles obtained in the Bahía de Tongoy (Ortega, 2014).