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Powering Earth’s dynamo with magnesium precipitation from the core

Author

Listed:
  • Joseph G. O’Rourke

    (California Institute of Technology)

  • David J. Stevenson

    (California Institute of Technology)

Abstract

The thermal conductivity of iron is now known to be much larger than had been thought, implying that thermal convection and radiogenic heating would not have been enough to sustain the Earth’s geodynamo; here it is shown that the precipitation of magnesium-bearing minerals from the core could have served as the required power source.

Suggested Citation

  • Joseph G. O’Rourke & David J. Stevenson, 2016. "Powering Earth’s dynamo with magnesium precipitation from the core," Nature, Nature, vol. 529(7586), pages 387-389, January.
  • Handle: RePEc:nat:nature:v:529:y:2016:i:7586:d:10.1038_nature16495
    DOI: 10.1038/nature16495
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    Cited by:

    1. Zhi Li & Kuangdai Leng & Jennifer Jenkins & Sanne Cottaar, 2022. "Kilometer-scale structure on the core–mantle boundary near Hawaii," Nature Communications, Nature, vol. 13(1), pages 1-8, December.

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