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Earth science

Missing link in mantle dynamics

The discovery of crystallographic imperfections known as disclinations in the most profuse mineral in Earth's upper mantle has the potential to solve a problem that has vexed mineral physicists for decades. See Article p.51

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Figure 1: Imaging polycrystalline olivine.

Sylvie Demouchy

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Correspondence to Greg Hirth.

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Hirth, G. Missing link in mantle dynamics. Nature 507, 42–43 (2014). https://doi.org/10.1038/nature13064

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