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From 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:scopusSeafloor margin map helps in understanding subduction earthquakes
ReviewAbstract:Palabras claves:Autores:Alexandra P. Alvarado, Jean Yves Collot, Lebrun J.F., Legonidec Y., Marcaillou B., Michaud F.A., Migeon S., Pazmino A., Schneider J.L., Sosson M., Spence G.Fuentes:scopus