At mid-ocean ridges, the directions in which plates spread and the underlying mantle flows were thought to broadly align. A synthesis of results from ridges that spread at a variety of rates reveals that instead there may be a systematic skew.
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Nedimović, M. Delayed response to mantle pull. Nature Geosci 9, 571–572 (2016). https://doi.org/10.1038/ngeo2746
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DOI: https://doi.org/10.1038/ngeo2746