Earthquakes track subduction fluids from their source in the slab to their sink in the mantle wedge
Felix Julian Halpaap1, Stephane Rondenay1, Alexander Perrin2, Saskia D B Goes3, Lars Ottemöller1, Florian Millet4, Håkon Austrheim5, Robert Shaw6 and Thomas Eeken7, (1)University of Bergen, Bergen, Norway, (2)Imperial College London, London, SW7, United Kingdom, (3)Imperial College London, Department of Earth Science and Engineering, London, United Kingdom, (4)LGLTPE Laboratoire de Géologie de Lyon : Terre, Planètes et Environnement, Villeurbanne Cedex, France, (5)University of Oslo, Oslo, Norway, (6)Imperial College London, London, United Kingdom, (7)Madison, WI, United States