Breakup reactions were used to study the ground-state configuration of the neutron-rich isotope 23 For decades the nuclear shell model has been one of the most important tools to interpret a wealth of experimental data. With the advent of radioactive-beam facilities, the evolution of nuclear shell structure far from the valley of stability could be studied. At present, such studies can be extended to the limits of bound nuclei on the neutron-rich side (the neutron dripline) for nuclear charges up to Z 8, oxygen. An important tool in this context are high-energy knockout reactions of single neutrons from near-dripline nuclei. Brown et al. [1] have shown that the residue momentum distributions and the corresponding cross sections can be analyzed in such a way that both the l values and the single-particle occupation probabilities of the levels can be deduced. This, however, requires that the level from which the breakup occurred is identified uniquely by measuring rays in coincidence with the residue [2,3].An interesting case to study is the series of neutronrich oxygen isotopes near the neutron dripline. As mentioned above, the experimental confirmation of such a theoretical analysis requires an exclusive knockout experiment where the individual levels are identified by measuring in coincidence the deexciting rays. We have performed such an exclusive experiment at the fragment separator FRS at Gesellschaft fü r Schwerionenforschung (GSI) in Darmstadt, Germany. The primary beam was 40 Ar at 1 GeV=nucleon delivered by the SIS synchrotron with an average intensity of 1:5 10 10 particles=spill.