Watching Dehydration: Seismic Indication for Transient Fluid Pathways in the Oceanic Mantle of the Subducting Nazca Slab
Author:
Affiliation:
1. Freie Universität Berlin; Berlin Germany
2. Deutsches GeoForschungszentrum; Potsdam Germany
3. Universidad Católica del Norte; Antofagasta Chile
4. National Research Center for Integrated Natural Disasters Management (CIGIDEN); Santiago Chile
Funder
Deutsche Forschungsgemeinschaft
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018GC007703/fullpdf
Reference95 articles.
1. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing;Audet;Nature,2009
2. Long-wave elastic anisotropy produced by horizontal layering;Backus;Journal of Geophysical Research,1962
3. Elasticity of antigorite, seismic detection of serpentinites, and anisotropy in subduction zones;Bezacier;Earth and Planetary Science Letters,2010
4. High-resolution image of the North Chilean subduction zone: Seismicity, reflectivity and fluids;Bloch;Geophysical Journal International,2014
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