In one case only (GRB 970508, Piro et al. 1998) did we find evidence of a spectral variation during the afterglow, correlated with the intensity. The source associated with this GRB rebursted with a hardening of the spectrum, and subsequently decayed with more rapid law and soft spectrum than that of all other afterglow sources. In the very beginning (Piro et al. 1999) we found evidence of an Fe line. This seems much more than a coincidence since the other burst which showed a rebursting behaviour (GRB 970828, Yoshida et al. 1998) shows as well evidence of an Fe line. In the frame of Synchrotron Shock models the re-acceleration of particles is possibly associated with the encounter of a relatively dense cloud of materials, which is also needed to interpret the Fe feature as fluorescence reprocessing of the primary X-rays from a circumburst environment.
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