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Oblique subduction modelling indicates along-trench tectonic transport of sediments

Author

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  • Cristina Malatesta

    (DISTAV, University of Genoa)

  • Taras Gerya

    (Institute of Geophysics, Swiss Federal Institute of Technology (ETH-Zurich))

  • Laura Crispini

    (DISTAV, University of Genoa)

  • Laura Federico

    (DISTAV, University of Genoa)

  • Giovanni Capponi

    (DISTAV, University of Genoa)

Abstract

Convergent plate margins are currently distinguished as ‘accretional’ or ‘erosional’, depending on the tendency to accumulate sediments, or not, at the trench. Accretion and erosion can coexist along the same margin and we have noticed that this mostly occurs where subduction is oblique. Here we show that at oblique subduction zones, sediments that enter the trench are first buried, and later migrate laterally parallel to the trench and at various depths. Lateral migration of sediments continues until they reach a physical barrier where they begin to accumulate. The accretionary wedge size decreases along the trench moving away from the barrier. We therefore suggest that the gradual variation of the accretionary wedge size and sediment amount at the trench along one single subduction zone, as observed in many active plate margins worldwide, can be explained by the lateral tectonic migration of sediments driven by obliquity of subduction as well.

Suggested Citation

  • Cristina Malatesta & Taras Gerya & Laura Crispini & Laura Federico & Giovanni Capponi, 2013. "Oblique subduction modelling indicates along-trench tectonic transport of sediments," Nature Communications, Nature, vol. 4(1), pages 1-6, December.
  • Handle: RePEc:nat:natcom:v:4:y:2013:i:1:d:10.1038_ncomms3456
    DOI: 10.1038/ncomms3456
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