Models indicate that there are strong gradients in element concentrations and in the pH of fluids at the slab–mantle interface — a major discontinuity deep within Earth. This transforms our view of global geochemical transport. See Letter p.420
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References
Galvez, M. E., Connolly, J. A. D. & Manning, C. E. Nature 539, 420–424 (2016).
Wilke, M. et al. Earth Planet. Sci. Lett. 349–350, 15–25 (2012).
Bernini, D., Wiedenbeck, M., Dolejš, D. & Keppler, H. Contrib. Mineral. Petrol. 165, 117–128 (2013).
Pan, D., Spanu, L., Harrison, B., Sverjensky, D. A. & Galli, G. Proc. Natl Acad. Sci. USA 110, 6646–6650 (2013).
Sverjensky, D. A., Harrison, B. & Azzolini, D. Geochim. Cosmochim. Acta 129, 125–145 (2014).
Dolejš, D. & Wagner, T. Geochim. Cosmochim. Acta 72, 526–553 (2008).
Galvez, M. E., Manning, C. E., Connolly, J. A. D. & Rumble, D. Earth Planet. Sci. Lett. 430, 486–498 (2015).
Frost, D. J. & McCammon, C. A. Annu. Rev. Earth Planet. Sci. 36, 389–420 (2008).
Evans, K. A., Elburg, M. A. & Kamenetsky, V. S. Geology 40, 783–786 (2012).
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Dolejš, D. Ions surprise in Earth's deep fluids. Nature 539, 362–364 (2016). https://doi.org/10.1038/539362a
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DOI: https://doi.org/10.1038/539362a