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Continental slope reconstruction after a giant mass failure, the example of the Matakaoa Margin, New Zealand
ArticleAbstract: During the Pleistocene, the Matakaoa Debris Avalanche (MDA) removed ~ 430 km3 of material and formedPalabras claves:debris-avalanche, mass-transport deposit, slope failure, slope reconstruction, submarine instability, TurbiditesAutores:Jean Yves Collot, Joanne C., Lamarche G., Migeon S.Fuentes:scopusEarthquake-triggered deposits in the subduction trench of the north Ecuador/south Colombia margin and their implication for paleoseismology
ArticleAbstract: The north Ecuador/south Colombia convergent margin is affected by recurrent subduction earthquakes wPalabras claves:210 Pb excess, Colombia trench, earthquakes, Levee, TurbiditesAutores:Garibaldi C., Jean Yves Collot, Migeon S., Ratzov G., Schmidt S., Texier L., Zaragosi S.Fuentes:scopusLate Quaternary geomorphologic evolution of submarine canyons as a marker of active deformation on convergent margins: The example of the South Colombian margin
ArticleAbstract: The morphology of Patia and Mira canyons on the South Colombian convergent margin reflects an interpPalabras claves:active tectonics, Convergent margins, submarine canyonAutores:Jean Yves Collot, Migeon S., Ratzov G., Sosson M.Fuentes:scopus