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Stable oxygen and hydrogen isotopic tracers in Amazon shelf waters during Amasseds ArchiMer
Karr, Jd; Showers, Wj.
A detailed hydrographic survey of the water column of the Amazon shelf was performed using stable oxygen and hydrogen isotopes to determine the source and fate of waters on the shelf. delta(18)O-H2O and deltaD measurements were made on water column samples from approximately 60 stations (three depths per station) which were each collected during four Amasseds (A Multidisciplinary Amazon Shelf SEDiment Study) cruises: I8909-August 1989, falling river discharge; I9002-March 1990, rising river discharge; I9004-May 1990, peak discharge: I9113-November 1991, minimum discharge. Isotopes were compared with salinity and temperature measurements in order to identify water masses and mixing. The characteristics (salinity, temperature, delta(18)O, deltaD and d) are...
Tipo: Text Palavras-chave: Amazone; Isotopes; 18O; Deutérium; Hydrologie; Amazon; Isotope; O-18; Deuterium; Hydrography.
Ano: 2002 URL: http://archimer.ifremer.fr/doc/00322/43321/42933.pdf
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Etude de la transition chenal-levées/lobe dans les systèmes turbiditiques récents. Application à l'éventail turbiditique de l'Amazone et au Néofan du Petit-Rhône ArchiMer
Jegou, Isabelle.
The channel-lobe transition zone has been studied in two turbiditic systems: the Amazon channel-mouth lobe complex at the termination of the last eight channel-levee systems and the Neochannel termination, the last active channel of the Petit-Rhone turbidite system. - In the two cases, the internal geometry and stacking pattern of the deposits show a significant control of the configuration (size and shape) of the receiving basins, their morphology (gradients and subtle gradient changes), and their degree of confinement. - The Amazon and Petit-Rhone systems, with lobes built after the Last Glacial Maximum and the ensuing sea-level rise, evidence the major impact of external forcings (climatic events and eustatic variations) that induce variations in...
Tipo: Text Palavras-chave: Post glacial deconnexion; Internal and external forcing parameters; Channel mouth lobe; Petit Rhone Neofan; Amazon Fan; Turbiditic systems; Déconnexion post glaciaire; Forçages internes et externes; Processus de compensation; Lobes terminaux; Néofan du Petit Rhône; Amazone; Systèmes turbiditiques.
Ano: 2008 URL: http://archimer.ifremer.fr/doc/2008/these-6796.pdf
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