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Evidence for hotspot-related carbonatite metasomatism in the oceanic upper mantle

Nature volume 365, pages 221–227 (1993)Cite this article

Abstract

Four peridotite xenoliths from the islands of Savai'i (Western Samoa) and Tubuai (Austral Islands) contain primary olivine of lithospheric origin, and secondary assemblages of clinopyroxene + spinel ± apatite. The trace-element contents of the secondary minerals show that they formed in equilibrium with carbonate-rich melts. Moreover, isotopic results indicate that these melts were derived from recycled crustal components in the convecting mantle, and place constraints on the origins of these components.

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Authors and Affiliations

  1. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, 02543, USA

    Erik H. Hauri, Nobumichi Shimizu & Stanley R. Hart

  2. Scripps Institution of Oceanography, Geological Research Division-0208, La Jolla, California, 92093, USA

    Julie J. Dieu

Authors
  1. Erik H. Hauri
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  2. Nobumichi Shimizu
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  3. Julie J. Dieu
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  4. Stanley R. Hart
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Hauri, E., Shimizu, N., Dieu, J. et al. Evidence for hotspot-related carbonatite metasomatism in the oceanic upper mantle. Nature 365, 221–227 (1993). https://doi.org/10.1038/365221a0

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