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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:scopusEstimation of successive coseismic vertical offsets using coeval sedimentary events-application to the southwestern limit of the Sea of Marmara's Central Basin (North Anatolian Fault)
ArticleAbstract: In the deep part of the Sea of Marmara (Turkey), the sedimentation developing upon the North AnatoliPalabras claves:Autores:Beck C., Cągatay N., Corina Campos, Eris K.K., Jouanne F., Mercier De Lepinay B.Fuentes:googlescopusStrain partitioning in the transition area between oblique subduction and continental collision, Hikurangi margin, New Zealand
ArticleAbstract: Spatial differences in late Quaternary structural style and deformation rates indicate a complex patPalabras claves:Autores:Audru J.C., Barnes P.M., Delteil J., Jean Yves Collot, Mercier De Lepinay B.Fuentes:scopus