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Article Dans Une Revue Seismological Research Letters Année : 2016

The Seismic Sequence of the 16 September 2015 M-w 8.3 Illapel, Chile, Earthquake

Sergio Ruiz
  • Fonction : Auteur
Emilie Klein
Francisco Del Campo
  • Fonction : Auteur
Efrain Rivera
  • Fonction : Auteur
Piero Poli
Christophe Vigny
  • Fonction : Auteur
Juan Carlos Baez
  • Fonction : Auteur
Gabriel Vargas
  • Fonction : Auteur
Felipe Leyton
  • Fonction : Auteur
Raul Madariaga
  • Fonction : Auteur
Luce Fleitout

Résumé

On 16 September 2015, the M-w 8.3 Illapel, Chile, earthquake broke a large area of the Coquimbo region of north-central Chile. This area was well surveyed by more than 15 high-rate Global Positioning System (GPS) instruments, installed starting in 2004, and by the new national seismological network deployed in Chile. Previous studies had shown that the Coquimbo region near Illapel was coupled to about 60%. After the M-w 8.8 Maule megathrust earthquake of 27 February 2010, we observed a large-scale postseismic deformation, which resulted in a strain rate increase of about 15% in the region of Illapel. This observation agrees with our modeling of viscous relaxation after the Maule earthquake. The area where upper-plate GPS velocity increased coincides very well with the slip distribution of the Illapel earthquake inverted from GPS measurements of coseismic displacement. The mainshock started with a small-amplitude nucleation phase that lasted 20 s. Backprojection of seismograms recorded in North America confirms the extent of the rupture, determined from local observations, and indicates a strong directivity from deeper to shallower rupture areas. The coseismic displacement shows an elliptical slip distribution of about 200 km x 100 km with a localized zone where the rupture is deeper near 31.3 degrees S. This distribution is consistent with the uplift observed in some GPS sites and inferred from field observations of bleached coralline algae in the Illapel coastal area. Most of aftershocks relocated in this study were interplate events, although some of the events deeper than 50 km occurred inside the Nazca plate and had tension (slab-pull) mechanisms. The majority of the aftershocks were located outside the 5 m contour line of the inferred slip distribution of the mainshock.
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Dates et versions

hal-02332004 , version 1 (24-10-2019)

Identifiants

Citer

Sergio Ruiz, Emilie Klein, Francisco Del Campo, Efrain Rivera, Piero Poli, et al.. The Seismic Sequence of the 16 September 2015 M-w 8.3 Illapel, Chile, Earthquake. Seismological Research Letters, 2016, 87 (4), pp.789-799. ⟨10.1785/0220150281⟩. ⟨hal-02332004⟩
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