Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean
Abstract Tsunamis are triggered by sudden seafloor displacements, and usually originate from seismic activity at faults. Nevertheless, strike-slip faults are usually disregarded as major triggers, as they are thought to be capable of generating only moderate seafloor deformation; accordingly, the ts...
Guardado en:
Autores principales: | , , , , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/70d328e119ca48878710bd9705a76a9c |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:70d328e119ca48878710bd9705a76a9c |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:70d328e119ca48878710bd9705a76a9c2021-12-02T15:08:10ZTsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean10.1038/s41598-021-95729-62045-2322https://doaj.org/article/70d328e119ca48878710bd9705a76a9c2021-08-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-95729-6https://doaj.org/toc/2045-2322Abstract Tsunamis are triggered by sudden seafloor displacements, and usually originate from seismic activity at faults. Nevertheless, strike-slip faults are usually disregarded as major triggers, as they are thought to be capable of generating only moderate seafloor deformation; accordingly, the tsunamigenic potential of the vertical throw at the tips of strike-slip faults is not thought to be significant. We found the active dextral NW–SE Averroes Fault in the central Alboran Sea (westernmost Mediterranean) has a historical vertical throw of up to 5.4 m at its northwestern tip corresponding to an earthquake of Mw 7.0. We modelled the tsunamigenic potential of this seafloor deformation by Tsunami-HySEA software using the Coulomb 3.3 code. Waves propagating on two main branches reach highly populated sectors of the Iberian coast with maximum arrival heights of 6 m within 21 and 35 min, which is too quick for current early-warning systems to operate successfully. These findings suggest that the tsunamigenic potential of strike-slip faults is more important than previously thought, and should be taken into account for the re-evaluation of tsunami early-warning systems.F. EstradaJ. M. González-VidaJ. A. PeláezJ. Galindo-ZaldívarS. OrtegaJ. MacíasJ. T. VázquezG. ErcillaNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-9 (2021) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Medicine R Science Q |
spellingShingle |
Medicine R Science Q F. Estrada J. M. González-Vida J. A. Peláez J. Galindo-Zaldívar S. Ortega J. Macías J. T. Vázquez G. Ercilla Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean |
description |
Abstract Tsunamis are triggered by sudden seafloor displacements, and usually originate from seismic activity at faults. Nevertheless, strike-slip faults are usually disregarded as major triggers, as they are thought to be capable of generating only moderate seafloor deformation; accordingly, the tsunamigenic potential of the vertical throw at the tips of strike-slip faults is not thought to be significant. We found the active dextral NW–SE Averroes Fault in the central Alboran Sea (westernmost Mediterranean) has a historical vertical throw of up to 5.4 m at its northwestern tip corresponding to an earthquake of Mw 7.0. We modelled the tsunamigenic potential of this seafloor deformation by Tsunami-HySEA software using the Coulomb 3.3 code. Waves propagating on two main branches reach highly populated sectors of the Iberian coast with maximum arrival heights of 6 m within 21 and 35 min, which is too quick for current early-warning systems to operate successfully. These findings suggest that the tsunamigenic potential of strike-slip faults is more important than previously thought, and should be taken into account for the re-evaluation of tsunami early-warning systems. |
format |
article |
author |
F. Estrada J. M. González-Vida J. A. Peláez J. Galindo-Zaldívar S. Ortega J. Macías J. T. Vázquez G. Ercilla |
author_facet |
F. Estrada J. M. González-Vida J. A. Peláez J. Galindo-Zaldívar S. Ortega J. Macías J. T. Vázquez G. Ercilla |
author_sort |
F. Estrada |
title |
Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean |
title_short |
Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean |
title_full |
Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean |
title_fullStr |
Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean |
title_full_unstemmed |
Tsunami generation potential of a strike-slip fault tip in the westernmost Mediterranean |
title_sort |
tsunami generation potential of a strike-slip fault tip in the westernmost mediterranean |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doaj.org/article/70d328e119ca48878710bd9705a76a9c |
work_keys_str_mv |
AT festrada tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT jmgonzalezvida tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT japelaez tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT jgalindozaldivar tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT sortega tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT jmacias tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT jtvazquez tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean AT gercilla tsunamigenerationpotentialofastrikeslipfaulttipinthewesternmostmediterranean |
_version_ |
1718388258375729152 |