Conditional Probabilities of Hellenic Arc Earthquakes Based on Different Distribution Models
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Pure and Applied Geophysics
Conditional Probabilities of Hellenic Arc Earthquakes Based on Different Distribution Models KAAN HAKAN COBAN1 Abstract—The 27 November 2019 Mw 6.0 earthquake that occurred in the southwestern part of the Hellenic Arc near Crete Island provided evidence of the high potential for strong earthquakes and active seismicity in the Hellenic Arc. In addition, tsunamis have been reported to occur for the region after major earthquakes in the historical past, so the seismic hazard of the Hellenic Arc should be evaluated in detail. The aim of this study is to evaluate the seismic hazard of the Hellenic Arc more reliably and accurately by estimating the conditional probabilities of a strong earthquake based on Weibull, gamma, log-normal, exponential, Rayleigh, and inverse Gaussian distribution models for the inter-event time of Mw C 6.0 earthquakes that occurred between 1900 and 2019 in the study area. The fit between each model and the data was tested using four different test criteria, namely the loglikelihood value, Akaike information criterion, Bayesian information criteria, and Kolmogorov–Smirnov test. According to the results, the inverse Gaussian distribution was selected as the best, the log-normal distribution as the second best, the Weibull and gamma distributions as intermediate, and the Rayleigh and exponential distribution as the poorest and second poorest model, respectively. The conditional probability of an earthquake with magnitude Mw C 6.0 is estimated to be higher than 0.70 according to all of the models used in this study for the base year te = 0 (te = 2015) and t [ 5 years (t [ 2020). Moreover, the results obtained based on the inverse Gaussian, exponential, log-normal, and Weibull distribution models are close to each other and are higher than 0.60 for te = 0 and t C 3 years (t C 2018). The outcomes of this study when using the different distribution models will contribute to assessments of the seismic as well as tsunami hazards for the region. Keywords: Hellenic Arc, seismic hazard, inverse Gaussian distribution, Weibull distribution, exponential distribution, tsunami hazard.
1. Introduction The Hellenic Arc forms one of the most active crustal-deforming parts of the Alpine–Himalayan
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Department of Geophysical Engineering, Karadeniz Technical University, Trabzon, Turkey. E-mail: [email protected]
and NILGUN SAYIL1 belt, which is related to its tectonic complexity and high seismicity. Therefore, many researchers have investigated the relationship between the complex tectonic structure and deformation of the Hellenic Arc in different tectonic, geodynamic, and seismological studies (e.g., Tsapanos et al. 1994; Taymaz et al. 1990, 1991, 2007; Becker et. al. 2006, 2010; Bohnhoff et al 2006; Shaw and Jackson 2010; Papanikolaou 2010; Confal et al. 2016; Bocchini et al. 2018). In addition, the deformation of the region has been evaluated by monitoring the movement of the Hellenic Arc with the help of GPS (e.g., McClusky et al. 2000; Reilinger et al. 2010). The complex tectonic
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