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Horizontal shear flow in the mantle beneath the Tonga arc

Abstract

In the Tonga subduction zone, a systematic shear deformation, in which deep material moves relatively to the south, is superimposed on the mode of down-dip shortening which is characteristic of the region. We interpret this observation, together with a tectonic reconstruction, in terms of the interaction between the subducting lithospheric slab and a horizontal shear flow in the mantle.

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Giardini, D., Woodhouse, J. Horizontal shear flow in the mantle beneath the Tonga arc. Nature 319, 551–555 (1986). https://doi.org/10.1038/319551a0

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