%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture non répertoriées par l'AERES
%A Pelletier, Bernard
%A Auzende, Jean-Marie
%T Geometry and structure of the Vitiaz trench lineament (SW Pacific)
%D 1996
%L fdi:010009466
%G ENG
%J Marine Geophysical Researches
%@ 0025-3235
%K TECTONIQUE DE PLAQUES ; SUBDUCTION ; CROUTE OCEANIQUE ; GEOLOGIE STRUCTURALE ; TECTONIQUE ; VOLCANISME ; BATHYMETRIE ; SISMIQUE A REFLEXION ; GEODYNAMIQUE
%K PACIFIQUE SUD OUEST ; VITIAZ REGION
%P 305-335
%R 10.1007/BF00286083
%U https://www.documentation.ird.fr/hor/fdi:010009466
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_6/b_fdi_45-46/010009466.pdf
%V 18
%W Horizon (IRD)
%X Swath bathymetric, sonar imagery and seismic reflection data dollected during thee SOPACMAPS cruise Leg 3 over segments of the Vitiaz Trench Lineament and adjacent areas provide new insights on the geometry and the structural evolution of this seismically inactive lineament. The Vitiaz Trench Lineament, although largely unknown, is one of the most important tectonic feature in the SW Pacific because it separates the Cretaceous crust of the Pacific Plate to the north from the Cenozoic lithosphere of the North Fiji and Lau Basins to the south. The lineament is considered to be the convergent plate boundary between the Pacific and Australian Plates during middle to late Tertiary time when the Vitiaz Arc was a continuous east-facing arc from the Tonga to the Solomon Islands before the development of the North Fiji and Lau Basins. Progresive reversal and cessation of subduction from west to east in the late Miocene-Lower Pliocene have been also proposed. However, precise structures and age of initiation and cessation of deformation along the Vitiaz Trench Lineament are unknown. The lineament consists of the Vitiaz Trench and three discontinuous and elongated troughs (Alexa, Rotuma and Horne Troughs) which connect the Vitiaz Trench to the northern end of the Tonga Trench. Our survey of the Alexa and Rotuma Troughs reveals that the lineament is composed of a series of WNW-ESE and ENE-WSW trending segments in front of large volcanic massifs belonging to the Melanesian Border Plateau, a WNW trending volcanic belt of seamounts and ridges on Pacific crust. The Plateau and Pacific plate lying immediately north of the lineament have been affected by intense normal faulting, collapse, and volcanism as evidenced by a series of tilted blocks, grabens, horsts and ridges trending N120° to N100° and N60°-70°. This tectonism includes several normal faulting episodes, the latest being very recent and possibly still active. (Résumé d'auteur)
%B Seafloor Mapping in the West and Southwest Pacific : Results and Applications
%8 1994/11/4-9
%$ 064TECTO