A model for a description of a shear crack (fault) propagation is proposed
on the basis of the unification of continuum damage and fracture mechanics
with ideas of Fracture models for random media. Energy release linked with
local failures of elements as a result of evolution of fracture processes a
t lower scale levels (stimulated by the stress concentration in the vicinit
y of the fault) is treated as a seismicity source. 2d simulations are perfo
rmed for analysis of the effect of the size of pre-existing fault on charac
teristic features of rupture evolution. Scaling (including multifractal) ch
aracter of crack propagation and of respective energy release is shown.