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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:scopusThe Rapuhia Scarp (northern Hikurangi Plateau) - Its nature and subduction effects on the Kermadec Trench
ArticleAbstract: Multibeam bathymetric data, seismic reflection and magnetic data are used to examine the nature of tPalabras claves:Hikurangi plateau subduction, Margin subsidence, tectonic erosionAutores:Davy B., Jean Yves CollotFuentes:scopus