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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:scopusDynamics of giant mass transport in deep submarine environments: The Matakaoa Debris Flow, New Zealand
ArticleAbstract: The Matakaoa Debris Flow (MDF) is a 200-km-long mass-transport deposit resulting from the failure ofPalabras claves:Autores:Jean Yves Collot, Joanne C., Lamarche G.Fuentes:scopusSuccessive, large mass-transport deposits in the south Kermadec fore-arc basin, New Zealand: The matakaoa submarine instability complex
ArticleAbstract: Four >100 km3 mass-transport deposits (MTDs) identified from their morphology and seismic facies acrPalabras claves:Debris avalanche, debris flow, Hikurangi Margin, Raukumara Basin, Slump, Submarine landslideAutores:Jean Yves Collot, Joanne C., Lamarche G.Fuentes:scopus