Resumen

LINKIMER, Lepolt et al. The 2016 Capellades earthquake and its seismic sequence: Expression of strike-slip faulting in the volcanic arc of Costa Rica. bol.geol. [online]. 2018, vol.40, n.2, pp.35-53. ISSN 0120-0283.  https://doi.org/10.18273/revbol.v40n2-2018002.

On 30 November 2016 at 18:25 (1st December at 00:25, UTC time) a Mw 5.5 earthquake occurred at 2.7 km depth, 4 km north of the town Capellades de Alvarado, Costa Rica. It was the main shock of an earthquake sequence including foreshocks and aftershocks, located 5 km from the active Irazú and Turrialba volcanoes. This is the most recent of a series of damaging earthquakes originated in the faults crossing the Central Volcanic Range, which constitutes the northern boundary of the most populated area of the country. Using mainly the seismic records from the National Seismological Network (RSN), we present in this study a seismological analysis of the earthquake sequence and the location and characteristics of the fault that originated this seismicity. Additionally, we describe the geotectonic context of the fault and the Capellades earthquake effects. The earthquake sequence shows a clear 8-km long alignment striking nor-northwest between Irazú and Turrialba volcanoes. The joint interpretation of the earthquake relocation, the main-shock moment tensor solution, and the focal mechanisms of 17 events allows for determining the source in a nearly vertical strike-slip fault, in agreement with regional active fault systems. This structure had not been recognized previously and has been named Liebres Fault in this study. The main shock was felt in most of the country, with a maximum intensity of VI+. This earthquake has been the largest in the eastern part of the Central Volcanic Range since the 1952 Patillos earthquake (Ms 5.9) and the first Mw > 5.0 earthquake recorded by the RSN in the Turrialba volcano edifice. Despite the proximity to this active volcano, which has been erupting periodically since 2010, there were no immediate eruptive effects.

Palabras clave : Liebres Fault; seismic sequence; focal mechanisms; tectonic in volcanoes; Turrialba Volcano.

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