upper stratified sequence and the lower unstratified sequence, respectively, which are
identified on the USGS profiles (Eittreim et al., 1984). Figure 8 shows the sedimentary basin
configuration on the TH82 profiles across the continental margin off Dumont d'Urville station,
on the basis of interpretation of the seismicreflection profiles described above. … The
marginal high that occurs along our survey line at the foot of the lower continental rise is …