The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran

Within two hours on 01 July 2023, three earthquakes of Mw 5.8-6.0 hit the SE Fars arc, Iran. In the following months, the region characterized by the collision of the Iranian and the Arabian plate, thrust faulting, and salt diapirism was stroke by more than 120 aftershocks of mL 3.1-5.2, of which tw...

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Main Authors: Malte Metz, Behnam Maleki Asayesh, Mohammad Mohseni Aref, Mohammadreza Jamalreyhani, Pınar Büyükakpınar, Torsten Dahm
Format: Article
Language:English
Published: McGill University 2023-11-01
Series:Seismica
Online Access:https://seismica.library.mcgill.ca/article/view/953
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author Malte Metz
Behnam Maleki Asayesh
Mohammad Mohseni Aref
Mohammadreza Jamalreyhani
Pınar Büyükakpınar
Torsten Dahm
author_facet Malte Metz
Behnam Maleki Asayesh
Mohammad Mohseni Aref
Mohammadreza Jamalreyhani
Pınar Büyükakpınar
Torsten Dahm
author_sort Malte Metz
collection DOAJ
description Within two hours on 01 July 2023, three earthquakes of Mw 5.8-6.0 hit the SE Fars arc, Iran. In the following months, the region characterized by the collision of the Iranian and the Arabian plate, thrust faulting, and salt diapirism was stroke by more than 120 aftershocks of mL 3.1-5.2, of which two of the largest events occurred within one minute on 23 July 2023 in spatial vicinity to each other. We analyzed both the large mainshocks and aftershocks using different techniques, such as the inversion of seismic and satellite deformation data in a joint process and aftershock relocation. Our results indicate the activation of thrust faults within the lower sedimentary cover of the region along with high aftershock activity in significantly larger depth, supporting the controversial model of a crustal strain decoupling during the collision in the Fars Arc. We resolved a magnitude difference of >0.2 magnitude units between seismic and joint seismic and satellite deformation inversions probably caused by afterslip, thereby allowing to bridge between results from international agencies and earlier studies. We also find evidence for an event doublet and triplet activating the same or adjacent faults within the sedimentary cover and the basement
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spelling doaj.art-1bb33d066405401894120c92fc6bfcff2023-11-16T18:31:53ZengMcGill UniversitySeismica2816-93872023-11-012210.26443/seismica.v2i2.953The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, IranMalte Metz0Behnam Maleki Asayesh1Mohammad Mohseni Aref2Mohammadreza Jamalreyhani3Pınar Büyükakpınar4Torsten Dahm5GFZ, German Research Center for Geosciences, PotsdamGFZ, German Research Centre for Geosciences, PotsdamUniversity of Potsdam, GermanyInstitute of Geophysics, University of Tehran, Tehran, IranGFZ, German Research Centre for Geosciences, Potsdam, GermanyGFZ German Research Centre for Geosciences, Potsdam, GermanyWithin two hours on 01 July 2023, three earthquakes of Mw 5.8-6.0 hit the SE Fars arc, Iran. In the following months, the region characterized by the collision of the Iranian and the Arabian plate, thrust faulting, and salt diapirism was stroke by more than 120 aftershocks of mL 3.1-5.2, of which two of the largest events occurred within one minute on 23 July 2023 in spatial vicinity to each other. We analyzed both the large mainshocks and aftershocks using different techniques, such as the inversion of seismic and satellite deformation data in a joint process and aftershock relocation. Our results indicate the activation of thrust faults within the lower sedimentary cover of the region along with high aftershock activity in significantly larger depth, supporting the controversial model of a crustal strain decoupling during the collision in the Fars Arc. We resolved a magnitude difference of >0.2 magnitude units between seismic and joint seismic and satellite deformation inversions probably caused by afterslip, thereby allowing to bridge between results from international agencies and earlier studies. We also find evidence for an event doublet and triplet activating the same or adjacent faults within the sedimentary cover and the basement https://seismica.library.mcgill.ca/article/view/953
spellingShingle Malte Metz
Behnam Maleki Asayesh
Mohammad Mohseni Aref
Mohammadreza Jamalreyhani
Pınar Büyükakpınar
Torsten Dahm
The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran
Seismica
title The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran
title_full The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran
title_fullStr The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran
title_full_unstemmed The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran
title_short The July-December 2022 earthquake sequence in the southeastern Fars arc of Zagros mountains, Iran
title_sort july december 2022 earthquake sequence in the southeastern fars arc of zagros mountains iran
url https://seismica.library.mcgill.ca/article/view/953
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