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Formation of forearc basins by collision between seamounts and accretionary wedges: an example from the New Hebrides subduction zone
ArticleAbstract: Seabeam data reveal two deep subcircular reentrants in the lower arc slope of the New Hebrides islanPalabras claves:Autores:Fisher M.A., Jean Yves CollotFuentes:scopusPossible causes for structural variation where the New Hebrides island arc and the d' Entrecasteaux zone collide.
ArticleAbstract: A major submarine mountain chain called the d'Entrecasteaux zone (DEZ) collides with the central parPalabras claves:Autores:Fisher M.A., Jean Yves Collot, Smith G.Fuentes:scopus