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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:scopusPrimary or secondary distal volcaniclastic turbidities: How to make the distinction? An example from the Miocene of New Zealand (Mahia Peninsula, North Island)
ArticleAbstract: Miocene marine volcaniclastic deposits occur in Mahia Peninsula (North Island, New Zealand) and werePalabras claves:Depositional process, Glass chemistry, Grain size, New zealand, Pyroclastic morphology, Volcaniclastic turbiditeAutores:Buret C., Chanier F., Ferrière J., Jean Noël Proust, Le Ruyet A., Rosseel J.B., Schneider J.L.Fuentes:scopus