Several pairs of planetary satellites may have been involved, during the hi
story of the Solar System, in mutual mass transfer processes. Such processe
s can be triggered by catastrophic collisions of a satellite (parent body)
with a third object. As a consequence, the collision fragments are injected
into independent orbits that can cross the trajectory of the another satel
lite (target). These swarms of secondary impacts may be of some importance
influencing the properties of the target body. Even the formation of the at
mosphere around some giant satellites may have been triggered by the gas re
leased after the impacts of fragments onto the target's surface. Moreover,
the different albedos and the different surface density of impact craters w
ithin the same satellite system may be connected to peculiar collisional ph
enomena, such as those we are dealing with. A quantitative modelling of the
role of mass transfer processes obviously requires an estimate of how much
material the parent bodies are able to supply, and under what circumstance
s the process may take place. A general analysis of the various pairs throu
ghout the major satellite systems present in the Solar System has been perf
ormed in the present paper. Our analysis uses a statistical algorithm, comp
uting, as a function of the initial properties of the fragments (masses and
ejection velocities from their parent body), the mean intrinsic probabilit
y of impact, and then the mean lifetime of a fragment before impacting the
target, as well as the distribution of the relative velocity. For an order-
of-magnitude estimate of the available amount of mass, some simple analytic
al equations have been derived to evaluate the fraction of fragments from t
he parent body that can reach the target. These formulae allow a preliminar
y discrimination of the interesting cases. The pair Hyperion-Titan and the
Uranus system have been analyzed in detail.