Abstract
A high-resolution bathymetric and seismic study of sinuous midfan channels on the Amazon Fan shows that some common elements of seismic profiles across the channel/levee system may be side echoes (sideswipe) from reflective, coarse channel-floor sediments Which lie to the side of the ship track. This includes portions of a dipping zone of high-amplitude reflectors beneath the channel. If these strong echoes are side echoes rather than buried coarse sediments, there may be less coarse material present within the midfan channel/levee systems than predicted, and channel evolution is still poorly resolved. Side echoes may be common in other areas of complex deep-sea morphology.
| Original language | English |
|---|---|
| Pages (from-to) | 15-22 |
| Number of pages | 8 |
| Journal | Geo-Marine Letters |
| Volume | 7 |
| Issue number | 1 |
| DOIs | |
| State | Published - Mar 1987 |
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