Active faulting, submarine surface rupture and seismic migration along the Liquiñe‐Ofqui fault system, Patagonian Andes
|Author(s)||Villalobos Angelo1, Vargas Easton Gabriel1, Maksymowicz Andrei2, Ruiz Sergio2, Lastras Galderic3, de Pascale Gregory P.1, Agurto‐detzel Hans4|
|Affiliation(s)||1 : Departamento de Geología, Facultad de Ciencias Físicas y MatemáticasUniversidad de Chile Santiago, Chile
2 : Departamento de Geofísica, Facultad de Ciencias Físicas y MatemáticasUniversidad de Chile Santiago ,Chile
3 : Grup de Recerca Consolidat en Geociències MarinesUniversitat de Barcelona Barcelona, Spain
4 : Université Côte d'Azur, IRD, CNRS, Observatoire de la Côte d'Azur, Géoazur Nice ,France
|Source||Journal Of Geophysical Research-solid Earth (2169-9313) (American Geophysical Union (AGU)), 2020-09 , Vol. 125 , N. 9 , P. e2020JB019946 (26p.)|
|WOS© Times Cited||9|
The intra‐arc Liquiñe‐Ofqui Fault System (LOFS) is an active transpressive fault zone located in the Patagonian Andes of Chile. In 2007, a seismic sequence occurred in the Aysén Fjord region of Chilean Patagonia along the LOFS, with a Mw 6.2 main earthquake that triggered dozens of landslides, some of which induced tsunami waves that caused severe damage and casualties. Through the analysis of high‐resolution seismic reflection and bathymetric data, we identify six submarine faults cutting the late‐Quaternary postglacial sedimentary infill of the fjord. The most conspicuous are the dextral‐normal NE‐SW‐striking Quitralco fault (QF) and the N‐S striking strike‐slip Río Cuervo (RCF) and Punta Cola faults (PCF). Our paleoseismological analysis reveals at least seven paleo‐landslide events buried in the fjord sediments, that were triggered by local paleoearthquakes, which occurred since local ice‐sheet retreat, i.e. ca. 12 kyrs. By combining tectonic observations with local seismicity data, we propose a seismotectonic model for the evolution of the 2007 seismic sequence where three structures were progressively activated from the depth towards the upper continental crust, causing surface rupture along the PCF and with earthquakes (i.e. partial ruptures along other faults). Because the other faults did not rupture to the seafloor they remain important sources of seismic hazard. Thus, the last seismic sequence was a consequence of a stress transfer from the lower‐ductile towards the upper‐brittle continental crust, close to the triple junction of the Nazca, South American and Antarctica Plates. Our results emphasize on the potential synergies between multiple geological and geophysical methods to assess complex events.
Plain Language Summary
When crustal faults rupture, the energy released are the earthquakes we feel at the surface of the Earth. Recent studies along strike‐slip faults, demonstrate that these phenomena are often not only related to a single fault, but instead take place along several faults like was seen in the 2016 Kaikoura earthquake in New Zealand. Using novel high‐resolution seismic reflection imagery and bathymetric data together with the reanalysis of local seismicity, we show (i) multiple active faults in the Aysén Fjord area along the Liquiñe‐Ofqui fault system in the Patagonian Andes, (ii) several of these faults were activated during the last 2007 seismic sequence and one of them (the Punta Cola fault), ruptured to the surface causing a Mw 6.2 earthquake that generated massive landslides and local tsunami, (iii) mapping of similar landslides in the fjord sediments demonstrates similar events occured at least seven times since the last ice‐sheet retreat in the area, i.e. in the last 12,000 years. This demonstrates the necessity for including the possibility of complex ruptures involving multiple faults regarding seismic hazard assessment along crustal faults, especially for faults near populated areas.