We discuss the pertinency of the log-Weibull model in the statistical under
standing of energy release for earthquake magnitude data. This model has ma
ny interesting features, the most remarkable of which being: depending on t
he value alpha > 0 of the deformation index of the source; it may present t
ails ranging from moderately heavy (alpha < 1) to very heavy (with tail ind
ex zero as alpha > 1): through hyperbolic (power law) for the critical valu
e a = 1. Under this model (fur which a precise tail study is supplied); the
occurrence of power laws appears as a critical phenomenon: this reinforces
the current tread predicting that some departure from the ideal (strictly
scaling fractal) model may be ubiquitous. Raving applied an affine transfor
mation in the logarithmic scale, quantile estimation and the Kolmogorov-Smi
rnov statistics are used to fit the log-Weibull distribution to a realizati
on of all iid sample. This enables to decide whether the upper tail of the
phenomenon under study is light/heavy/very heavy. A comparative study of re
corded French and Japanese earthquake magnitudes suggests that they exhibit
comparable tail behaviour; albeit with different centrality and dispersion
parameters.