Références des communications dans des colloques internationaux
Hamelin, C., Dosso, L., Moreira, M., Hanan, B., Kositsky, A. P., (2010), Geochemical portray of the Pacific ridge using statistical techniques,Geochimica et Cosmochimica Acta, Volume 74, Issue 11 Supplement 1, A373.
Moreira, MA; Gayer, E; Guillon, F, Dosso, L., Ondréas, H., 2009. Rare gases on off-axis seamounts: Constraints on the marble-cake model. Goldschmidt Conference, Davos, Suisse. Geochimica et Cosmochimica Acta Vol: 73, Issue: 13, pp A903-A903
Dosso, L., Hamelin, C., Hanan, B, Moreira, M., Barrat, J.-A. (2007). Geochemical segmentation of the Pacific-Antarctic Ridge. Goldschmidt Conference, Cologne, Allemagne.
Briais A., Ondréas H., Klingelhoefer F., Dosso L., Guillou H., 2006. Analysis of off-axis volcanic ridges on the flank of the Pacific-Antarctic ridge. Results from the Pacantarctic 2 cruise. European Geosciences Union 2006, 2-7 april 2006, Vienna, Austria, Geophysical Research abstracts, 8, 04323.
C. Hamelin, L.Dosso, B. Hanan, M. Moreira, J.-A. Barrat, Scales of Geochemical Segmentation of the Pacific Ridge, American Geophysical Union, Fall Meeting 2006, abstract #V31D-0619.
Ondréas H., Klingelhoefer F., Briais A., Hamelin C., Dosso L., 2006. The Pacific - Antarctic ridge between 41°S and 53°S: hot underlying mantle evidenced by bathymetry and gravity studies coupled to geochemical results. European Geosciences Union 2006, 2-7 april 2006, Vienna, Austria, Geophysical Research abstracts, 8, 03397.
Briais A., Ondréas H., Klingelhoefer F., Dosso L., 2005. Analysis of off-axis volcanic ridges on the flanks of the Pacific- Antarctic Ridge. Results from Pacantarctic 2 cruise. AGU Fall Meeting. Abstract in, EOS Transaction, 86, 52.
Hamelin C., Dosso L., Hanan B.B., Moreira M., Klingelhoefer F., Barrat J., Ondréas H., 2005. The Pacific - Antarctic Ridge axis between 41° and 51°S: first sampling and geochemical data. AGU Fall Meeting. Abstract in, EOS Transaction, 86, 52.
Ondréas H., Klingelhoefer F., Briais A., Hamelin C., Dosso L., 2005. The Pacific - Antarctic Ridge between 41° S and 51°S: hot underlying mantle evidenced by bathymetry and gravity studies coupled to geochemical results. AGU Fall Meeting. Abstract in, EOS Transaction, 86, 52.