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...
Main Authors: | , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | French |
Published: |
Société Géologique de France
1978
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Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/1978/publication-5228.pdf https://archimer.ifremer.fr/doc/00000/5228/ |