Clustering Analysis of Seismicity in the Anatolian Region with Implications for Seismic Hazard

The Anatolian region is one of the most seismically active tectonic settings in the world.
Here, we perform a clustering analysis of Turkish seismicity using an updated version of the Turkish
Homogenized Earthquake Catalogue (TURHEC), which contains the recent developments of the
still ongoing Kahramanmaras seismic sequence. We show that some statistical properties of seismic
activity are related to the regional seismogenic potential. Mapping the local and global coefficients
of variation of inter-event times of crustal seismicity which occurred during the last three decades,
we find that territories prone to major seismic events during the last century usually host globally
clustered and locally Poissonian seismic activity. We suggest that regions with seismicity associated
with higher values of the global coefficient of variation of inter-event times, CV, are likely to be more
prone to hosting large earthquakes in the near future than other regions characterized by lower values,
if their largest seismic events have the same magnitude. If our hypothesis is confirmed, clustering
properties should be considered as a possible additional information source for the assessment of
seismic hazard. We also find positive correlations between global clustering properties, the maximum
magnitude and the seismic rate, while the b-value of the Gutenberg–Richter law is weakly correlated
with them. Finally, we identify possible changes in such parameters before and during the 2023
Kahramanmara¸s seismic sequence.

One comment

  1. Dear Davide,

    I hope this email finds you well. I am Hamza Skikra, a Ph.D. student in structural geology currently researching the structural evolution of the High Atlas region in Morocco. I recently came across your intriguing research on seismic clustering analysis in the Anatolian region, and I was impressed by your work with the Turkish Homogenized Earthquake Catalogue (TURHEC).
    Given the seismic activity in the High Atlas, particularly the September M7 earthquake, I believe there is a valuable opportunity for collaboration between our areas of expertise. I am eager to contribute to a similar research initiative for the Moroccan Earthquake using my background in structural geology, including field observations, paleostress data, and other relevant structural information.
    Your expertise in seismicity analysis would complement the understanding of the seismotectonic features in the High Atlas. I am confident that our collaboration could yield meaningful insights into the active tectonics of the region.

    Best regards,

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