Fig. 19From: Statistical study on the regional characteristics of seismic activity in and around Japan: frequency-magnitude distribution and tidal correlationComparison of the observed FMDs with those expected from the L-L formula (Eq. 7) using the best-fit parameters. \(M\) data corresponding to the typical \(b\)-value and typical \(\eta\)-value PDDs are used for each \(N\) and \(l\) pair. a Area A; b area BBack to article page