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scopus(16)
Characterizing earthquake recurrence parameters for offshore faults in the low-strain, compressional Kapiti-Manawatu Fault System, New Zealand
ArticleAbstract: Seafloor fault scarps and near-surface deformation of late Quaternary seismic reflectors occur alongPalabras claves:Autores:Jean Noël Proust, Lamarche G., Nodder S.D., Stirling M.Fuentes:scopusClimate and Tectonic Changes in the Ocean Around New Zealand
ArticleAbstract:Palabras claves:Autores:Jean Noël Proust, Lamarche G., Niwa H.N.Fuentes:scopusBuilding an 18 000-year-long paleo-earthquake record from detailed deep-sea turbidite characterisation in Poverty Bay, New Zealand
ArticleAbstract: Two ∼20 m-long sedimentary cores collected in two neighbouring mid-slope basins of the Paritu TurbidPalabras claves:Autores:Jean Noël Proust, Lamarche G., Pouderoux H.Fuentes:scopusContinental 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:scopusAbrupt strike-slip fault to subduction transition: The alpine fault-puysegur trench connection, New Zealand
ArticleAbstract: Swath bathymetry and other geophysical data collected over the Fiordland Margin, southwest of New ZePalabras claves:Autores:Delteil J., Jean Yves Collot, Lamarche G., Lebrun J.F.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:scopusFrom oblique subduction to intra-continental transpression: Structures of the southern Kermadec-Hikurangi margin from multibeam bathymetry, side-scan sonar and seismic reflection
ArticleAbstract: The southern Kermadec-Hikurangi convergent margin, east of New Zealand, accommodates the oblique subPalabras claves:Multibeam bathymetry, Oblique subduction, Seamount collision, Strike-slip faults, Tectonic accretion, tectonic erosion, Transpressive deformationAutores:Audru J.C., Barnes P.M., Chanier F., Chaumillon E., Davy B., Delteil J., Jean Yves Collot, Lallemand S.E., Lamarche G., Lewis K.B., Mercier De Lepinay B., Orpin A., Pelletier B., Sosson M., Toussaint B., Uruski C.Fuentes:scopusFrom strike-slip faulting to oblique subduction: A survey of the Alpine Fault-Puysegur Trench transition, New Zealand, results of cruise Geodynz-sud leg 2
ReviewAbstract: The Geodynz-sud cruise on board the R/V l'Atalante collected bathymetric, side-scan sonar and seismiPalabras claves:New zealand, Oblique subduction, Puysegur ridge, Puysegur trench, Strike-slip, Swath bathymetryAutores:Calmant S., Christoffel D., Coffin M., Delteil J., Ferrière J., Herzer R.H., Jean Yves Collot, Lamarche G., Lebrun J.F., Mauffret A., Pontoise B., Popoff M., Ruellan E., Sosson M., Sutherland R., Wood R.A.Fuentes:scopusSubduction initiation at a strike-slip plate boundary: The Cenozoic Paciic-Australian plate boundary, south of New Zealand
ArticleAbstract: We first present a synthesis of the Macquarie Ridge Complex (MRC) tectonic structures as well as palPalabras claves:Australia, Cenezoic, Macquarie Ridge, Pacific, Plate motion, Subduction initiationAutores:Jean Yves Collot, Lamarche G., Lebrun J.F.Fuentes:scopusSubmarine paleoseismology of the northern Hikurangi subduction margin of New Zealand as deduced from Turbidite record since 16ka
ArticleAbstract: Paleoseismic studies seek to characterise the signature of pre-historical earthquakes by deriving quPalabras claves:Active margin, Earthquake hazard assessment, Paleoearthquake, Peak ground acceleration, Poverty Bay, Synchronous slope failures, Turbidite paleoseismologyAutores:Jean Noël Proust, Lamarche G., Pouderoux H.Fuentes:scopus