Rupture Segmentation of the 14 August 2021 Mw 7.2 Nippes, Haiti, Earthquake Using Aftershock Relocation from a Local Seismic Deployment

Author:

Douilly Roby1ORCID,Paul Sylvert234ORCID,Monfret Tony245ORCID,Deschamps Anne24ORCID,Ambrois David24ORCID,Symithe Steeve J.34ORCID,St Fleur Sadrac3,Courboulex Françoise24ORCID,Calais Eric246ORCID,Boisson Dominique34ORCID,de Lépinay Bernard Mercier24ORCID,Font Yvonne24ORCID,Chèze Jérôme24ORCID

Affiliation:

1. 1Department of Earth and Planetary Sciences, University of California, Riverside, Riverside California, U.S.A.

2. 2Université Côte d’Azur, CNRS, IRD, Observatoire de la Côte d’Azur, Géoazur, France

3. 3Faculté des Sciences, Unité de Recherche en Géosciences (URGeo), Port-au-Prince, Haiti

4. 4CARIBACT Joint Research Laboratory, Port-au-Prince, Haiti

5. 5Barcelona Center for Subsurface Imaging, Institut de Ciències del Mar (ICM), CSIC, Barcelona, Spain

6. 6Department of Geosciences, Ecole Normale Supérieure, Paris, France

Abstract

ABSTRACT The 14 August 2021 Mw 7.2 Haiti earthquake struck 11 yr after the devastating 2010 event within the Enriquillo Plantain Garden (EPG) fault zone in the Southern peninsula of Haiti. Space geodetic results show that the rupture is composed of both left-lateral strike-slip and thrust motion, similar to the 2010 rupture; but aftershock locations from a local short-period network are too diffuse to precisely delineate the segments that participated in this rupture. A few days after the mainshocks, we installed 12 broadband stations in the epicentral area. Here, we use data from those stations in combination with four local Raspberry Shakes stations that were already in place as part of a citizen seismology experiment to precisely relocate 2528 aftershocks from August to December 2021, and derive 1D P- and S-crustal velocity models for this region. We show that the aftershocks delineate three north-dipping structures with different strikes, located to the north of the EPG fault. In addition, two smaller aftershock clusters occurred on the EPG fault near the hypocenter area, indicative of triggered seismicity. Focal mechanisms are in agreement with coseismic slip inversion from Interferometric Synthetic Aperture Radar data with nodal planes that are consistent with the transpressional structures illustrated by the aftershock zones.

Publisher

Seismological Society of America (SSA)

Subject

Geochemistry and Petrology,Geophysics

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