Abstract
THE development of subduction zones may depend on the motion of the two converging lithospheric plates relative to the underlying deep mantle. It is likely that the plates move much more rapidly than the underlying mantle1–4, the return flow being diffused through a large region1,5. The deep mantle is thus nearly stationary and the horizontal motion of sinking plates that extend to depths of 700 km must be significantly restrained.
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HYNDMAN, R. Plate Motions relative to the Deep Mantle and the Development of Subduction Zones. Nature 238, 263–265 (1972). https://doi.org/10.1038/238263b0
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DOI: https://doi.org/10.1038/238263b0
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