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( Geophysical study of the Chesterfield Plateau (SW Pacific); Preliminary results of the ZOE200 cruise ( R/V Coriolis)).
ArticleAbstract: The Chesterfield Plateau is a highstanding feature located near the N termination of the Lord Howe RPalabras claves:Autores:Jean Yves Collot, Missegue F.Fuentes:scopus( Gravimetric anomalies and crustal structure in the new Caledonia area: the roots of the peridotites).
ArticleAbstract: Studies of the E border of New Caledonia and the deep structure of the Loyalty Basin establish the cPalabras claves:Autores:Jean Yves Collot, Malahoff A., Missegue F.Fuentes:scopusFracture zone subduction and reactivation across the Puysegur ridge/trench system, southern New Zealand
ArticleAbstract: A two-dimentional kinematic model for lithospheric thrusting that considers the flexural interactionPalabras claves:Autores:Jean Yves Collot, Karner G.D., Lebrun J.F.Fuentes:scopusGeologic structure of the northern New Caledonia Ridge, as inferred from magnetic and gravity anomalies
ArticleAbstract: Bathymetric, gravity, and magnetic data collected in the southwest Pacific Ocean over the northern NPalabras claves:Autores:ègue F., Jean Yves Collot, Rigolot P.Fuentes:scopusFirst results of SUBPSO I dives in the collision zone "Loyalty Islands ridge/New Hebrides island arc', South West Pacific
ArticleAbstract: Four dives were conducted over the collision zone "Loyalty ridge/New Hebrides arc'. On the Loyalty rPalabras claves:Autores:Boulin J., Daniel J., Jean Yves Collot, Lallemand S.E., Monzier M., Pelletier B.Fuentes:scopusInfluence of preexisting backstop structure on oblique tectonic accretion: The Fiordland margin (southwestern New Zealand)
ArticleAbstract: The thinned continental crust of the Australian plate is being obliquely subducted beneath the SouthPalabras claves:Autores:Delteil J., Herzer R.H., Jean Yves Collot, Lebrun J.F., Sosson M., Wood R.A.Fuentes:scopusStrain partitioning in an accretionary wedge, in oblique convergence: Analogue modelling
ArticleAbstract: In subduction zones undergoing oblique convergence, strain partitioning is often expressed by an impPalabras claves:Accretionary wedge, Analog model, Coulomb wedge, Oblique convergence, Slip vector, Strain partitioning, Strike-slip faultAutores:Jean Yves Collot, Lallemand S.E., Malavielle J., Martinez A.Fuentes:scopusStrain partitioning in the transition area between oblique subduction and continental collision, Hikurangi margin, New Zealand
ArticleAbstract: Spatial differences in late Quaternary structural style and deformation rates indicate a complex patPalabras claves:Autores:Audru J.C., Barnes P.M., Delteil J., Jean Yves Collot, Mercier De Lepinay B.Fuentes:scopusStructure of the collision zone between Bougainville Guyot and the accretionary wedge of the New Hebrides Island Arc, southwest Pacific
ArticleAbstract: Multichannel seismic reflection data show the structure that develops within an island arc‐guyot colPalabras claves:Autores:Fisher M.A., Geist E., Jean Yves CollotFuentes:scopusThe dammed Hikurangi Trough: A channel-fed trench blocked by subducting seamounts and their wake avalanches (New Zealand-France GeodyNZ Project)
ArticleAbstract: The Hikurangi Trough, off eastern New Zealand, is at the southern end of the Tonga-Kermadec-HikurangPalabras claves:Autores:Jean Yves Collot, Lallemand S.E., Lewis K.B.Fuentes:scopus