Numerical comparison of different convergent plate contacts: subduction channel and subduction fault

Details Numerical comparison of different convergent plate contacts: subduction channel and subduction fault Numerical comparison of different convergent plate contacts: subduction channel and subduction fault

Oct 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007geoji.171..435d&link_type=abstract

Geophysical Journal International, Volume 171, Issue 6, pp. 435-450.

Astronomy and Astrophysics

Astronomy

9

Backarc Deformation, Fault, Numerical Modelling, Plate Contact, Subduction, Subduction Channel

Scientific paper

At convergent plate boundaries, the properties of the actual plate contact are important for the overall dynamics. Convergent plate boundaries both mechanically decouple and link tectonic plates and accommodate large amounts of strain. We investigate two fundamental physical states of the subduction contact: one based on a fault and the other based on a subduction channel. Using a finite element method, we determine the specific signatures of both states of the subduction contact. We pay particular attention to the overriding plate. In a tectonic setting of converging plates, where the subducting plate is freely moving, the subduction channel reduces compression relative to the fault model. In a land-locked basin setting, where the relative motion between the far field of the plates is zero, the subduction channel model produces tensile stress regime in the overriding plate, even though the amount of slab roll-back is small. The fault model shows a stronger development of slab roll-back and a compressive stress regime in the upper plate. Based on a consistent comparison of fault and channel numerical models, we find that the nature of the plate contact is one of the controlling factors in developing or not of backarc extension. We conclude that, the type of plate contact plays a decisive role in controlling the backarc state of stress. To obtain backarc extension, roll-back is required as an underling geodynamic process, but it is not always a sufficient condition.

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