Plio-Quaternary sedimentation on the Wilkes land continental rise: preliminary results
The Wilkes Land continental rise is characterised by mounds and channels with approximately a north–south elongation, perpendicular to the margin. Proximal mound relief is up to 1000 m, decreasing to about 300 m in the central part. During the geophysical and geological survey conducted on in Februa...
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Veröffentlicht in: | Deep-sea research. Part II, Topical studies in oceanography Topical studies in oceanography, 2003-05, Vol.50 (8), p.1529-1562 |
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