Co- and postseismic subaquatic evidence for prehistoric fault activity near Coyhaique, Aysén Region, Chile

Abstract. Chilean Patagonia is confronted with several geohazards due to its tectonic setting, i.e., the presence of a subduction zone and numerous fault zones, e.g., the Liquiñe-Ofqui Fault Zone (LOFZ). This region has therefore been the subject of numerous paleoseismological studies. However, this study reveals that the seismic hazard is not limited to these large tectonic structures by identifying past fault activity near Coyhaique in Aysén Region. Mass-wasting deposits in Lago Pollux, a lake located ca. 15 km SW of this region's capital, were identified through analysis of reflection-seismic data and were linked to a simultaneous event recorded in nearby Lago Castor. Furthermore, a coeval ∼50-year-long catchment response was identified in Aysén Fjord based on the multiproxy analysis of a portion of a sediment core. Assuming that this widely recognized event was triggered by an earthquake, ground-motion modeling was applied to derive the most likely magnitude and source fault. The model showed that an earthquake rupture along a local fault, in the vicinity of Lago Pollux and Lago Castor, with a magnitude of 5.6–6.8, is the most likely scenario.

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Publication Details

Journal
Natural hazards and earth system sciences
Published
2024-10-07
DOI
https://doi.org/10.5194/nhess-24-3401-2024
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
0.00

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article

Co- and postseismic subaquatic evidence for prehistoric fault activity near Coyhaique, Aysén Region, Chile

Catherine Kissel, Katleen Wils, Roberto Urrutia, Mario Pino et al.
Natural hazards and earth system sciences
earthquake and tectonic studies
article

Co- and postseismic subaquatic evidence for prehistoric fault activity near Coyhaique, Aysén Region, Chile

Catherine Kissel, Katleen Wils, Roberto Urrutia, Mario Pino, Morgan Vervoort, Marc De Batist, Kris Vanneste, Maarten Van Daele
article en

Abstract

Abstract. Chilean Patagonia is confronted with several geohazards due to its tectonic setting, i.e., the presence of a subduction zone and numerous fault zones, e.g., the Liquiñe-Ofqui Fault Zone (LOFZ). This region has therefore been the subject of numerous paleoseismological studies. However, this study reveals that the seismic hazard is not limited to these large tectonic structures by identifying past fault activity near Coyhaique in Aysén Region. Mass-wasting deposits in Lago Pollux, a lake located ca. 15 km SW of this region's capital, were identified through analysis of reflection-seismic data and were linked to a simultaneous event recorded in nearby Lago Castor. Furthermore, a coeval ∼50-year-long catchment response was identified in Aysén Fjord based on the multiproxy analysis of a portion of a sediment core. Assuming that this widely recognized event was triggered by an earthquake, ground-motion modeling was applied to derive the most likely magnitude and source fault. The model showed that an earthquake rupture along a local fault, in the vicinity of Lago Pollux and Lago Castor, with a magnitude of 5.6–6.8, is the most likely scenario.

Natural hazards and earth system sciencesVol. 24(10)
Centre National de la Recherche Scientifique (FR), United Nations Economic Commission for Latin America and the Caribbean (CL), Austral University of Chile (CL), University of Concepción (CL), Université de Versailles Saint-Quentin-en-Yvelines (FR), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), Royal Observatory of Belgium (BE), Ghent University (BE), Laboratoire des Sciences du Climat et de l'Environnement (FR), CEA Paris-Saclay (FR)
European Commission, Centro Euro-Mediterraneo sui Cambiamenti Climatici, Fonds Wetenschappelijk Onderzoek, Universiteit Gent, Vlaamse regering
Life below water
Openalex Percentile: Top 82%
earthquake and tectonic studies
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