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Figure 4. Bathymetry of the eastern Manus Basin, from multibeam data compiled by Institut francàis de rescherche pour l'exploitation de la mer (IFREMER). The southeast-trending Djaul transform is conspicuous. The northeast trending deep on the western side is a failed spreading segment. PACMANUS lies at the crest of a northeast trending ridge of dacite (Pual Ridge).

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