Influence des courants profonds sur les faciès sédimentaires du Vema Channel (Atlantique sud) à la fin du Cénozoïque

The sediments of six cores from the Rio Grande Rise side of the Vema Channel reflect major phases in the sedimentary history of this area since Ihe lower Miocene. Cores taken from below the present-day lysocline (approx. 4 000 m) consist essentially of calcareous oozes. The variable degree of preser...

Full description

Bibliographic Details
Main Authors: Melguen, Marthe, Debrabant, Pierre, Chamley, Hervé, Maillot, Henry, Hoffert, Michel, Courtois, Chantal
Format: Article in Journal/Newspaper
Language:French
Published: Société Géologique de France 1978
Subjects:
Online Access:https://archimer.ifremer.fr/doc/1978/publication-5228.pdf
https://archimer.ifremer.fr/doc/00000/5228/