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Implications for metal and volatile cycles from the pH of subduction zone fluids

Author

Listed:
  • Matthieu E. Galvez

    (Swiss Federal Institute of Technology)

  • James A. D. Connolly

    (Swiss Federal Institute of Technology)

  • Craig E. Manning

    (Planetary and Space Sciences, University of California)

Abstract

A thermodynamic model of fluid pH and its variability in Earth’s mantle and subducting crust highlights chemical feedbacks that connect deep Earth to surface processes.

Suggested Citation

  • Matthieu E. Galvez & James A. D. Connolly & Craig E. Manning, 2016. "Implications for metal and volatile cycles from the pH of subduction zone fluids," Nature, Nature, vol. 539(7629), pages 420-424, November.
    • Handle: RePEc:nat:nature:v:539:y:2016:i:7629:d:10.1038_nature20103
    DOI: 10.1038/nature20103
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    Cited by:

    1. Seohee Yun & Huijeong Hwang & Gilchan Hwang & Yeongkyoo Kim & Douglas Blom & Thomas Vogt & Jeffrey E. Post & Tae-Yeol Jeon & Tae Joo Shin & Dong-Zhou Zhang & Hiroyuki Kagi & Yongjae Lee, 2022. "Super-hydration and reduction of manganese oxide minerals at shallow terrestrial depths," Nature Communications, Nature, vol. 13(1), pages 1-8, December.

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