Abstract
This report summarizes and analyses the seafloor reflectivity characteristics along the northwest African margin between 3oN and 23oN. The reflectivity characteristics and microphysiography show that both downslope processes and along- slope processes have been important in shaping the present morphology of the continental rise.-from Author
| Original language | English |
|---|---|
| Pages (from-to) | 31-46 |
| Number of pages | 16 |
| Journal | Bulletin - Institut de Geologie du Bassin d'Aquitaine |
| Volume | 31-32 |
| State | Published - 1982 |
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