Elodie Marchès, Thierry Mulder, Eliane Gonthier, Michel Cremer, Thierry Garlan
The N-S Portimao Canyon on the Algarve Margin (N. Gulf of Cadiz) captures the E-W flowing Mediterranean Outflow Water. On the eastern side of the canyon, the MOW builds thick prograding elongated separated drift (including a moat), made of silty contourites and a strong sedimentation rate. On the western side of the canyon, the MOW builds thin aggrading drift made of muddy contourites and a low sedimentation rate.
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