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The March 2021 seismic sequence in Larisa - Damasi , Thessaly (central Greece), its seismotectonic characteristics and geodynamic effects

Authors :
Ganas, Athanassios
Valkaniotis, Sotiris
Tsironi, Varvara
Karasante, Ilektra
Elias, Panagiotis
Kapetanidis, Vassilis
Kasssaras, Ioannis
Papathanassiou, George
Briole, Pierre
Laboratoire de géologie de l'ENS (LGENS)
Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)
Publication Year :
2021
Publisher :
Zenodo, 2021.

Abstract

On March 3, 2021 a Mw=6.3 shallow earthquake occurred in the mountainous region of Damasi, about 20 km to the northwest of Larisa, Thessaly, central Greece, in a region of active crustal extension but of low strain. This event was followed by a Mw=6.0 shallow earthquake on March 4, 2021 about 12 km to the northwest, inside the sedimentary basin of the Titarisios river. On March 12, 2021 a third event of Mw=5.6 occurred 7 km further towards NNW, near the NW edge of the basin. All events show normal-slip kinematics as indicated by the moment tensor solutions, with minor strike-slip components. Because of the shallow depth of the events it was possible to map the surface deformation using InSAR. The preliminary results from InSAR show three main lobes of subsidence, partially overlapping. The deformation pattern indicates the activation of three normal faults, previously unknown in this part of Thessaly. The earthquakes generated numerous secondary phenomena with vast areas of alluvial deposits exhibiting spectacular liquefaction features. No tectonic ruptures were found in the cases of events 2 and 3, however a series of sporadic, NW-SE striking surface breaks were found on the mountains north of village Zarko that are aligned with the vanishing gradient of the interferometric phase of the 1st event. &nbsp

Details

Language :
English
Database :
OpenAIRE
Accession number :
edsair.doi.dedup.....1f38c1245fcd66db63ff551e32d77955
Full Text :
https://doi.org/10.5281/zenodo.4617264