Relocation of the 8 September 2023 High Atlas, Morocco, Earthquake Aftershock Sequence

ABSTRACT The earthquake that occurred on 8 September 2023, with a magnitude of 6.8, was the most destructive earthquake event in Morocco in the past decade. This earthquake took place in the Al Haouz region, located in the western part of the High Atlas Mountain range. To better understand what caused and triggered this earthquake, the earthquake catalogs including P and S arrival times were collected from the Moroccan seismic network and combined with regional data from the International Seismological Centre. The mainshock and aftershocks were relocated by using iLoc, a state-of-the-art single-event location algorithm, and then by the multiple event location double-difference algorithm, hypoDD. The improved earthquake relocations using iLoc and the double-difference methods provide sharper lineation of seismicity and agree well with tomographic images of the earthquake zone. The seismicity distribution and the focal mechanism of the mainshock indicate that the earthquake sequence has occurred along the South Atlas fault system.

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Publication Details

Journal
Bulletin of the Seismological Society of America
Published
2024-10-31
DOI
https://doi.org/10.1785/0120240100
Citations
5
Primary Topic
earthquake and tectonic studies
Type
article
Field-Weighted Citation Impact
2.67
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Relocation of the 8 September 2023 High Atlas, Morocco, Earthquake Aftershock Sequence

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Bulletin of the Seismological Society of America
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Relocation of the 8 September 2023 High Atlas, Morocco, Earthquake Aftershock Sequence

Lahcen Hni, Istvan Bondár, Andrea Chiang, Youssef Timoulali, Mohamed Kasmi
article en
5 citations

Abstract

ABSTRACT The earthquake that occurred on 8 September 2023, with a magnitude of 6.8, was the most destructive earthquake event in Morocco in the past decade. This earthquake took place in the Al Haouz region, located in the western part of the High Atlas Mountain range. To better understand what caused and triggered this earthquake, the earthquake catalogs including P and S arrival times were collected from the Moroccan seismic network and combined with regional data from the International Seismological Centre. The mainshock and aftershocks were relocated by using iLoc, a state-of-the-art single-event location algorithm, and then by the multiple event location double-difference algorithm, hypoDD. The improved earthquake relocations using iLoc and the double-difference methods provide sharper lineation of seismicity and agree well with tomographic images of the earthquake zone. The seismicity distribution and the focal mechanism of the mainshock indicate that the earthquake sequence has occurred along the South Atlas fault system.

Bulletin of the Seismological Society of AmericaVol. 115(5)
Lawrence Livermore National Laboratory (US), Centre National pour la Recherche Scientifique et Technique (CNRST) (MA)
Sustainable cities and communities
Openalex Percentile: Top 10%
earthquake and tectonic studies
2.67
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