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Seismology

Earthquake of the month: Samos-Izmir earthquake

Earthquake of the month: Samos-Izmir earthquake

On October 30th, a strong earthquake with Mw 7.0 occurred in the Aegean Sea, between the main cities of Samos in Greece and Izmir in Turkey. The hypocenter location and focal mechanism suggest shallow depth (~10 km) and normal faulting on the E-W plane. This is in agreement with the tectonic setting where an N-S extension is dominant. Moreover, the rupture propagates near the Menderes Graben in Western Turkey, a region of historical strike-slip and normal faulting (Figure 1, Karasözen et al., 20161).

Figure 1 | Tectonic setting and location of the Samor-Izmir earthquake (red star). Credits: Sylvain Barbot @quakephysics2

Preliminary InSAR analyses show that most of the deformation appears to be underwater (Figure 2). Also, it reflects uplift of about 5-10 cm in western Samos Island, and a small area of the coast subsided due to the earthquake. This strong gradient between uplift and subsidence in Samos Island observed with InSAR data could be a key point to better understand the fault mechanism of this earthquake. However further models, analysis, and field evidence are needed.

Figure 2 | Map of ground displacements calculated from Sentinel-1 radar by NASA-JPL ARIA project3.

Some regional and teleseismic finite-fault models are available (Figure 3). Most of them show likely bilateral shallow rupture with maximum slip around 2 to 3 meters. Despite the bilateral rupture, the slip seems to propagate mostly west-ward followed by aftershock seismicity. A different source time function shows that the rupture propagates for ~20 seconds. However, it is important to keep in mind that finite fault models can not constrain a preferred fault plane properly, due to the ambiguity between the fault and auxiliary planes obtained from the focal mechanism. To discriminate between each nodal plane it is necessary to assess and compare with more data, e.g. InSAR or other geodetical methods.

Figure 3 | Slip distribution model using as initial rupture of the hypocenter  (from KOERI4), the methodology proposed by Shimizu et al., 20205, and two possible fault planes (USGS, W-phase Moment Tensor6). Credits: Ryo Okuwaki @rokuwaki7

 

Normal faults can trigger a localized tsunami, and that was observed only a few minutes after the earthquake (Figure 4). Coastal cities close to seismogenic sources only have a short time window to activate the Tsunami Early Warning System to warn the population.

 

Figure 4 | Simulation of tsunami wave propagation in the Aegean Sea. Credits: (TOP) Amir Salaree @amirsalaree8, (BOTTOM) Jorge Macías Sánchez @JorgeMACSAN9

 

The Samor-Izmir earthquake caused significant damage in populated cities, for example, the impact in Izmir results in a peak ground acceleration (PGA) close to 1g in the horizontal component (Figure 5). The high PGA resulted in the collapse of buildings, numerous fatalities, and missing people.

 

Figure 5 | Acceleration in a near field record. Station GMLD, network KO. Credits: Iunio Iervolino @iuniervo10


 

TOP 3 – October earthquakes
Sand Point earthquake (Alaska) – 19th October – M 7.6
Samos-Izmir earthquake (Greece/Turkey) – 30th October – M 7.0
Pangai earthquake (Tonga) – 30th October – M 6.4


 

References

    • 1 Karasözen, E., Nissen, E., Bergman, E. A., Johnson, K. L., & Walters, R. J. (2016). Normal faulting in the Simav graben of western Turkey reassessed with calibrated earthquake relocations. Journal of Geophysical Research: Solid Earth, 121(6), 4553-4574
    • 2 https://twitter.com/quakephysics/status/1322242343198621696/photo/1
    • 3 https://appliedsciences.nasa.gov/what-we-do/disasters/disasters-activations/aegean-sea-earthquake-october-2020
    • 4 http://www.koeri.boun.edu.tr/new/en
    • 5 Shimizu, K., Yagi, Y., Okuwaki, R., & Fukahata, Y. (2020). Development of an inversion method to extract information on fault geometry from teleseismic data. Geophysical Journal International, 220(2), 1055-1065.
    • 6 https://earthquake.usgs.gov/earthquakes/eventpage/us7000c7y0/executive
    • 7 https://twitter.com/rokuwaki/status/1322697505499394048/photo/1
    • 8 https://twitter.com/amirsalaree/status/1322541828214726656/video/1
    • 9 https://twitter.com/JorgeMACSAN/status/1322199843100643328/photo/1
    • 10 https://twitter.com/iuniervo/status/1322211934972895233/photo/1

 

This blog post was written by ECS representative Javier Ojeda
with revisions from ECS representative Maria Tsekhmistrenko

EGU Seismology ECS Team
We are a team coming from mixed places with various interests: Janneke does her DPhil in DIAS, Dublin and is the Seismology ECS point of contact. Javier joint recently from Chile and is doing his DPhil in DGF, Universidad de Chile. Eric is finishing up his DPhil in Vienna, Austria and takes care of our Twitter account. Michaela is doing her DPhil in ETH, Swiss. Maria is doing her first PostDoc in DIAS, Dublin and since recently she is the editor-in-chief for the blog. Nienke hangs around in the University of Cambridge, UK and Walid is starting a PostDoc in Washington University in St Louis, US.


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