Activité magmatique, tectonique et hydrothermale actuelle sur la Dorsale Est Pacifique entre17°-et 19°S(campagne NAUDUR)

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Éditeur(s) Gauthier-villars
Identifiant documentaire 9-29458
Identifiant OAI oai:archimer.ifremer.fr:29458
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Auteur(s): Auzende, Jean-marie,Ballu, Valerie,Batiza, R,Bideau, Daniel,Cormier, Mh,Fouquet, Yves,Geistdoerfer, Patrick,Lagabrielle, Yves,Sinton, J,Spadea, P
Mots clés Océan Pacifique Dorsale ultra-rapide Magmatisme Tectonique Hydrothermalisme. PACIFIC OCEAN ULTRA-FAST SPREADING RIDGE MAGMATISM TECTONICS HYDROTHERMALISM
Date de publication 01/10/1994
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Langue fre
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Source Comptes Rendus de l'Academie des Sciences Serie II (1251-8069) (Gauthier-villars), 1994-10 , Vol. 319 , N. 7 , P. 811-818
Droits de réutilisation Académie des Sciences

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Description
The submersible-study of four segments of the East Pacific Rise between 17 degrees and 18 degrees 40'S, where the spreading rate is greater than 150 mm/a, allows us to confirm the variability of the accretion processes. The segment between 17 degrees and 17 degrees 30'S shows an intense present-day magmatic activity. The one between 18 degrees 10' and 18 degrees 22'S shows a mainly tectonic activity. The segment between 18 degrees 22' and 18 degrees 37'S is an intermediate stage with an axial graben in which fresh lavas were emplaced by an extremely young eruption. On all the segments the hydrothermal activity exists ranging from shimmering water up to black smokers, It is associated with different stages of animal colonization.

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