We present results on the formation of buried silicide layers at ion implan
tation doses in the range of 1-60% of the critical dose for formation of a
uniform layer We emphasize observations for the low-dose range of 1-5% wher
e the precipitate density is quite dilute. The Co redistribution during pos
t-implant annealing is measured using Rutherford backscattering techniques
and secondary ion mass spectrometry. Experimental observations during posti
mplantation annealing at 1000 degrees C involves (i) a contraction of the C
o depth profile for all doses, (ii) shifting of the peak of the profile tow
ards the hulk, and (iii) formation of a secondary Co peak near the surface.
The secondary peak is only present in samples implanted to greater than 3%
of the critical dose. The interpretation of the shift of the main peak and
the occurrence of the secondary peak requires a model exceeding the standa
rd ripening model used previously to describe mesotaxy. We suggest that mor
e recent ripening-based concepts allow for a full description of these obse
rvations with a minimum of parameters, particularly not requiring interacti
on with the complex defect profiles formed initially during implantation. E
ssential for this model is a proper inclusion of precipitate-precipitate in
teractions and the role of diffusion screening.