Seismicity and state of stress within the overriding plate of the Tonga-Kermadec subduction zone

Author:

Bonnardot M.-A.1,Régnier M.1,Ruellan E.1,Christova C.2,Tric E.1

Affiliation:

1. Université Nice-Sophia Antipolis, Institut de Recherche pour le Développement (I.R.D.), Centre National de Recherche Scientifique (CNRS); Laboratoire Geosciences Azur; Valbonne; France

2. Department of Seismology; Geophysical Institute of Bulgarian Academy of Sciences; Sofia; Bulgaria

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference55 articles.

1. Stress trajectories and relative motion at consuming boundaries: The Hellenic subduction (Greece) and the Philippine-Eurasia collision (Taiwan and Japan) as examples;Angelier;C. R. Hebd. Seances. Acad. Sci.,1982

2. Subduction of a late Cretaceous seamount of the Louisville Ridge at the Tonga trench: A model of normal and accelerated tectonic erosion;Ballance;Tectonics,1989

3. Morphology and history of the Kermadec trench-arc-backarc basin-remnant arc system at 30 to 32°S: Geophysical profile, microfossil and K-Ar data;Ballance;Mar. Geol.,1999

4. Geodetic observations of very rapid convergence and back-arc extension at the Tonga arc;Bevis;Nature,1995

5. Bonnardot , M.-A. 2006 Etude geodynamique de la zone de subduction Tonga-Kermadec par une approche couplee de modelisation numerique 3D et de sismotectonique/Geodynamical study of the Tonga-Kermadec subduction zone using both 3-D numerical modelling and seismotectonics approaches Univ. Nice-Sophia Antipolis Nice, France

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