From oblique subduction to intra-continental transpression: Structures of the southern Kermadec-Hikurangi margin from multibeam bathymetry, side-scan sonar and seismic reflection

Article

Abstract: The southern Kermadec-Hikurangi convergent margin, east of New Zealand, accommodates the oblique sub

Palabras claves:

Multibeam bathymetry, Oblique subduction, Seamount collision, Strike-slip faults, Tectonic accretion, tectonic erosion, Transpressive deformation

Autores:

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:

scopus