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Pathway from subducting slab to surface for melt and fluids beneath Mount Rainier

Author

Listed:
  • R. Shane McGary

    (MS#22, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, Massachusetts 02543, USA)

  • Rob L. Evans

    (MS#22, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, Massachusetts 02543, USA)

  • Philip E. Wannamaker

    (Energy and Geoscience Institute, University of Utah, 423 Wakara Way, Suite 300, Salt Lake City, Utah 84108, USA)

  • Jimmy Elsenbeck

    (MS#22, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, Massachusetts 02543, USA)

  • Stéphane Rondenay

    (University of Bergen, Allegaten 41, 5007 Bergen, Norway)

Abstract

Magnetotelluric data from the state of Washington, USA, are used to image the fluid–melt phase of volcanic subduction in Mt Rainier, revealing fluid release at or near the top of the slab, and its migration into the overlying mantle.

Suggested Citation

  • R. Shane McGary & Rob L. Evans & Philip E. Wannamaker & Jimmy Elsenbeck & Stéphane Rondenay, 2014. "Pathway from subducting slab to surface for melt and fluids beneath Mount Rainier," Nature, Nature, vol. 511(7509), pages 338-340, July.
    • Handle: RePEc:nat:nature:v:511:y:2014:i:7509:d:10.1038_nature13493
    DOI: 10.1038/nature13493
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    Cited by:

    1. Junxing Chen & Hehe Jiang & Ming Tang & Jihua Hao & Meng Tian & Xu Chu, 2022. "Venus’ light slab hinders its development of planetary-scale subduction," Nature Communications, Nature, vol. 13(1), pages 1-9, December.

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