La fracture Gibbs et la circulation profonde en Atlantique Nord

The cold waters from the Norwegian Sea are the main source of the underflow system in the northern Atlantic Ocean (10) (pl. 1, fig. 1b). The role of these currents in the formation of large sediment ripples has been demonstrated in some recent studies [(2), (3)]. As in the southern Atlantic Ocean, t...

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Bibliographic Details
Main Authors: Olivet, Jean-louis, Le Pichon, Xavier, Laubier, Lucien
Format: Article in Journal/Newspaper
Language:French
Published: Académie des Sciences 1970
Subjects:
Online Access:https://archimer.ifremer.fr/doc/1970/publication-4882.pdf
https://archimer.ifremer.fr/doc/00000/4882/