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Showing 1–5 of 5 results
Advanced filters: Author: Philip E. Wannamaker Clear advanced filters

  • Newly forming subduction zones on Earth can provide insights into the evolution of major fault zone geometries from shallow levels to deep in the lithosphere, and into the role of fluids in promoting rock failure by several modes. The acquisition of a transect of magnetotelluric soundings across the Marlborough strike–slip fault system of the northern South Island of New Zealand now implicates three distinct processes connecting fluid generation along the upper mantle plate interface to rock deformation in the crust as the subduction zone develops.

    • Philip E. Wannamaker
    • T. Grant Caldwell
    • Wiebke Heise
    Research
    Nature
    Volume: 460, P: 733-736

  • Where the Pacific and Australian tectonic plates collide under the South Island of New Zealand large quantities of aqueous fluid are produced. But how does this happen? Geophysical and petrological data indicate that it may not be as we thought.

    • Philip E. Wannamaker
    News & Views
    Nature Geoscience
    Volume: 3, P: 10-11

  • 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.

    • R. Shane McGary
    • Rob L. Evans
    • Stéphane Rondenay
    Research
    Nature
    Volume: 511, P: 338-340