Advanced statistical methodologies have been applied to detect temporal and
spatial scaling-invariance laws in seismicity observed in a seismogenetic
area of the Southern Apennine chain, which in past and recent years was dev
astated by destructive events. A deeper analysis of the seismicity observed
in this area during the period 1983-1995 is presented. A counting statisti
cal procedure has been applied to highlight scaling laws in the time domain
and a fractal approach has been carried out to reveal spatial self-similar
ity. The main features of the dynamic system under study have been depicted
using the key parameters of the more recurrent scaling laws observed in th
e spatial and temporal domains and we point out that the seismotectonic env
ironment of the Southern Apennine chain can be considered as an extended di
ssipative system. The comparative analysis of different dynamical parameter
s of earthquake sequences provides a more comprehensive evaluation of seism
otectonic processes in the investigated area.