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Melt-rich channel observed at the lithosphere–asthenosphere boundary

Author

Listed:
  • S. Naif

    (Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego)

  • K. Key

    (Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego)

  • S. Constable

    (Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego)

  • R. L. Evans

    (Woods Hole Oceanographic Institution)

Abstract

Sea-floor magnetotelluric data are used to image the electrical conductivity of the lithosphere–asthenosphere boundary offshore of Nicaragua; a high-conductivity layer confined to depths of 45–70 kilometres is found, interpreted to be a partially molten channel of low viscosity.

Suggested Citation

  • S. Naif & K. Key & S. Constable & R. L. Evans, 2013. "Melt-rich channel observed at the lithosphere–asthenosphere boundary," Nature, Nature, vol. 495(7441), pages 356-359, March.
    • Handle: RePEc:nat:nature:v:495:y:2013:i:7441:d:10.1038_nature11939
    DOI: 10.1038/nature11939
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    Cited by:

    1. Xin Wang & Ling Chen & Kelin Wang & Qi-Fu Chen & Zhongwen Zhan & Jianfeng Yang, 2024. "Seismic evidence for melt-rich lithosphere-asthenosphere boundary beneath young slab at Cascadia," Nature Communications, Nature, vol. 15(1), pages 1-10, December.
    2. Suraj K. Bajgain & Aaron Wolfgang Ashley & Mainak Mookherjee & Dipta B. Ghosh & Bijaya B. Karki, 2022. "Insights into magma ocean dynamics from the transport properties of basaltic melt," Nature Communications, Nature, vol. 13(1), pages 1-10, December.

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