E. De-oseberg-1, Application d'un délai en tempsàtempsà la source de 51.2 ms

. En-terme-de-complexité, nous considérons le champ de Oseberg comme un milieu simple localement complexe, Même si le champ de vitesse est globalement 1D, nous savons que la partie 16.2. DONNÉESDONN´DONNÉES HYDRATECH 203

B. Ces-multiplesétantmultiplesétant-sous-le, nous n'avons pas essayé de les atténuer. La qualité de la section est altérée par la présence de nombreux pics dans les traces

B. Le, . La, and . Tokai, Une caractéristique du BSR dans cette région est la présence d'un double BSR, 2003.

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D. Dans-nos, un seul BSR (tiret orange de la zone 2 sur la figure 16.36) clairement identifiable. Ce BSR estparalì ele et de signe opposé au fond de l'eaù a une distance horizontale comprise entre 20 et 30 kilomètres. Il est bien visible sous le haut de la pente, puis dispara??tdispara??t en bas de celle-ci

. Fig, 36 ? Position du BSR (tiret orange) dans la zone 2. Position de l'´ evénementevénementà forte amplitude, nonparalì ele et de même signe que le fond de l'eau (tiret-point vert) dans la zone

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