Abstract:A b s t r a c tThe Iranian Plateau does not appear to be a single crustal block, but an assemblage of zones comprising the Alborz-Azerbaijan, Zagros, Kopeh-Dagh, Makran, and Central and East Iran. The Gumbel's III asymptotic distribution method (GIII) and maximum magnitude expected by Kijko-Sellevoll method is applied in order to check the potentiality of the each seismogenic zone in the Iranian Plateau for the future occurrence of maximum magnitude (M max ). For this purpose, a homogeneous and complete seismi… Show more
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