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Young formation age of a mantle plume source

Nature volume 362, pages 715–721 (1993)Cite this article

Abstract

The Ninetyeast Ridge hotspot track displays strontium, neodymium and lead isotope variations over time that reflect simple radioactive decay in the plume source rather than a change in the mantle components present. The lead isotope variations indicate that the time spent by the plume source in a non-convecting mantle boundary layer was only a few hundreds of millions of years, contrary to the conventional view of individual plume sources as old (1–3 Gyr) or persistent features.

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Author information

Authors and Affiliations

  1. Max-Planck-lnstitut für Chemie, Postfach 3060, W-6500, Mainz, Germany

    Cornelia Class, Steven L. Goldstein, Stephen J. G. Galer & Dominique Weis

  2. Université Libre de Bruxelles, 50 Avenue F. D. Roosevelt, B-1050, Brussels, Belgium

    Dominique Weis

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  1. Cornelia Class
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  2. Steven L. Goldstein
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  3. Stephen J. G. Galer
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  4. Dominique Weis
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Class, C., Goldstein, S., Galer, S. et al. Young formation age of a mantle plume source. Nature 362, 715–721 (1993). https://doi.org/10.1038/362715a0

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