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A tear fault boundary between the Taiwan orogen and the Ryukyu subduction zone
ArticleAbstract: More than twenty seismic lines were analysed across the intersection of the Taiwan orogen and the RyPalabras claves:Arc-continent collision, Coastal Range of Taiwan, Ryukyu subduction zone, Subsidence, TAIWÁN, Tear faultAutores:Lallemand S.E., Liu C.S., Yvonne FontFuentes: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:scopusThe dammed Hikurangi Trough: A channel-fed trench blocked by subducting seamounts and their wake avalanches (New Zealand-France GeodyNZ Project)
ArticleAbstract: The Hikurangi Trough, off eastern New Zealand, is at the southern end of the Tonga-Kermadec-HikurangPalabras claves:Autores:Jean Yves Collot, Lallemand S.E., Lewis K.B.Fuentes:scopus