Experiments on silicon diffusion in the mineral olivine cast doubt on the widely held belief that water has a significant effect on the rheological properties of Earth's upper mantle. See Letter p.213
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References
Griggs, D. T. & Blacic, J. D. Science 147, 292–295 (1965).
Kohlstedt, D. L. Rev. Miner. Geochem. 62, 377–396 (2006).
Fei, H., Wiedenbeck, M., Yamazaki, D. & Katsura, T. Nature 498, 213–215 (2013).
Regenauer-Lieb, K., Yuen, D. A. & Branlund, J. Science 294, 578–580 (2001).
Moresi, L. & Solomatov, V. Geophys. J. Int. 133, 669–682 (1998).
Korenaga, J. J. Geophys. Res. 116, B12403 (2011).
Girard, J., Chen, J., Raterron, P. & Holyoke, C. W. Phys. Earth Planet. Inter. 216, 12–20 (2013).
Bercovici, D. & Ricard, Y. Phys. Earth Planet. Inter. 202–203, 27–55 (2012).
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Brodholt, J. Water may be a damp squib. Nature 498, 181–182 (2013). https://doi.org/10.1038/498181a
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DOI: https://doi.org/10.1038/498181a