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

R. Shane McGary (), Rob L. Evans, Philip E. Wannamaker, Jimmy Elsenbeck and Stéphane Rondenay
Additional contact information
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

Nature, 2014, vol. 511, issue 7509, 338-340

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.

Date: 2014
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DOI: 10.1038/nature13493

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