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Geochemistry

Ions surprise in Earth's deep fluids

Nature volume 539, pages 362364 (17 November 2016) | Download Citation

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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Affiliations

  1. David Dolejš is at the Institute of Earth and Environmental Sciences, University of Freiburg, 79104 Freiburg, Germany.

    • David Dolejš

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Correspondence to David Dolejš.

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DOI

https://doi.org/10.1038/539362a

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