## 5 Concluding Remarks  
In summarizing the study's findings, we concentrated on analyzing the distributions of interevent times for each sequence in order to statistically examine its patterns in the most recent aftershock sequences in Greece.  
Namely:  
* We can state that the aftershock sequences located in Greece follows the statistical mechanics model derived in the framework of Non-Extensive Statistical Physics (NESP);
* Moreover, we should note that the NESP approach is useful for other regions, not only for the Greek territory, such as subduction zones all over the word [53];
* According to the NESP approach used here, it suggests that the system is in an abnormal equilibrium with a transition for large interevent times from abnormal (\(q>1\)) to normal (\(q=1\)) statistical mechanics;
* The analysis of the interevent times distribution indicates such a system;
* The range of the non-extensive parameter \(q\) and for all sequences studied, results in a non-extensive entropic parameter \(q\) with a range of between 1.62 and 1.71, which suggests a system with one degree of freedom.  
To summarize, the used models fit the noticed distributions reasonably well, and imply the importance of using NESP in evaluating such phenomena.  
The main limitations of the work presented in this paper are related to earthquakes in different geotectonic environments along with fault types of the main shock. Studying aftershock sequences as a function of geotectonic environments is a matter of discussion in future studies, and this could be useful for the prediction of damaged aftershocks [54; 55; 56; 57].  
Conceptualization, F.V.; methodology, F.V., E.-A., S.-E.A., G.M.; software, G.M. and E.-A.A.; validation, E.-A.A. and S.-E.A.; formal analysis, F.V., E.-A.A., S.-E.A., G.M.; investigation, F.V., E.-A.A., S.-E.A., G.M.; resources, F.V., E.-A.A., S.-E.A., G.M.; data curation, F.V., E.-A.A., S.-E.A., G.M.; writing--original draft preparation, F.V., E.-A.A., S.-E.A., G.M.; writing--review and editing, F.V., E.-A.A., G.M.; visualization, F.V., E.-A.-A.; supervision, F.V. All authors have read and agreed to the published version of the manuscript.  
This research received no external funding.  
Data Availability Statement: Data are available at the Hellenic Unified Seismic Network (H.U.S.N., [[http://www.gein.noa.gr/en/networks/husn](http://www.gein.noa.gr/en/networks/husn)]([http://www.gein.noa.gr/en/networks/husn](http://www.gein.noa.gr/en/networks/husn))), (A.U.TH.: Aristothe University of Thessaloniki [[[http://geophysics.geo.auth.gr/ss/](http://geophysics.geo.auth.gr/ss/)]([http://geophysics.geo.auth.gr/ss/](http://geophysics.geo.auth.gr/ss/))], E.M.S.C.: European Mediterranean Seismological Centre [[[https://www.emsc-csem.org/#2](https://www.emsc-csem.org/#2)]([https://www.emsc-csem.org/#2](https://www.emsc-csem.org/#2))], N.K.U.A.: National and Kapodistrian University of Athens [[[http://www.geophysics.geol.uoa.gr/](http://www.geophysics.geol.uoa.gr/)]([http://www.geophysics.geol.uoa.gr/](http://www.geophysics.geol.uoa.gr/))], K.O.E.R.I.: Kandilli Observatory and Earthquake Research Institute [[[http://www.koeri.boun.edu.tr/new/en](http://www.koeri.boun.edu.tr/new/en)]([http://www.koeri.boun.edu.tr/new/en](http://www.koeri.boun.edu.tr/new/en))]. Last visit to the above webpages: 12 September 2022.  
We would like to thank [PERSON] for his valuable assistance in the construction of the seismotectonic map.  
The authors declare no conflict of interest.