The breakup of a projectile oxygen nucleus on a proton into multiply charge
d fragments has been investigated at an incident energy of 3.25 GeV/c per p
rojectile nucleon, and new experimental data from this investigation are pr
esented. In collisions where the fragments retain the charge of the inciden
t nucleus, only channels involving fragments with even charges are observed
. Among these, there are always helium nuclei, whose total yield is dominat
ed by the He-4 isotope, which contributes about 85%. For collisions where t
he fragments also retain the total number of constituent nucleons, final st
ates are formed either by four alpha particles or by an alpha particle and
a C-12 nucleus.