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a b l e asymptotic distribution calculated by least China circles indicate maximum coefficient H values earthquake occurrence earthquakes constructed estimating the parameters European Seismological Commission exponential and Johnson extreme magnitudes extreme values four models Gibowicz Gumbel Third Gumbel Gumbel Triple exponential indicate maximum magnitudes induced seismicity intervals Tix Jablonna Johnson distribution Johnson model Kraków large earthquakes largest values least squares method likelihood function magni maximum likelihood method maximum magnitudes observed Mean return period methods of estimation mining tremors missed values natural seismicity observed every month periods for magnitudes plotting rule Poland precision coefficient predicted return periods region removing the trend seismic hazard seismogram Table Third Gumbel distribution third Gumbel model Third Gumbel Triple trend calculated Triple exponential distribution Triple exponential Johnson triple exponential model tude Turkey values of H Wanganui area Warszawa Wujek Xi G(x д д д