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Astron. Astrophys. 333, 1082-1091 (1998) ![]() Available formats: HTML | PDF | (gzipped) PostScript Modelling the disruption and reaccumulation of Miranda
F. Marzari 1,
E. Dotto 1,
D.R. Davis 2,
S.J. Weidenschilling 2 and
V. Vanzani 1
Received 25 September 1997 / Accepted 12 January 1998 Abstract The heavily cratered surfaces of the largest Uranian satellites and the unusual surface geology of Miranda suggest that Miranda could have been catastrophically disrupted by collision and then reaccumulated over solar system history (Smith et al., 1986; McKinnon et al., 1991). Using the numerical model described by Marzari et al. (1995) we have simulated the breakup of Miranda by a high velocity impact and computed the size and orbital distributions of the collisional fragments. These distributions have been adopted as realistic initial conditions for the numerical algorithm of Spaute et al. (1991) with which we have simulated the reaccumulation of the satellite from the ring of debris. Our results show that the reaccumulation of Miranda occurs on a
short timescale ( Different breakup reaccumulation scenarios have been analyzed to account for the variation of some physical parameters. Key words: Miranda Send offprint requests to: F. Marzari © European Southern Observatory (ESO) 1998 Online publication: April 28, 1998 ![]() |