Deep slab hydration induced by bending-related variations in tectonic pressure
- 11 October 2009
- journal article
- Published by Springer Science and Business Media LLC in Nature Geoscience
- Vol. 2 (11), 790-793
- https://doi.org/10.1038/ngeo656
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- Upper lithospheric structure of the subduction zone offshore of southern Arauco peninsula, Chile, at ∼38°SJournal of Geophysical Research, 2008
- Seismicity in the outer rise offshore southern Chile: Indication of fluid effects in crust and mantleEarth and Planetary Science Letters, 2008
- Passive and active seismological study of bending-related faulting and mantle serpentinization at the Middle America trenchEarth and Planetary Science Letters, 2007
- Thermal cracking and the deep hydration of oceanic lithosphere: A key to the generation of plate tectonics?Journal of Geophysical Research, 2007
- Relationship between bend‐faulting at trenches and intermediate‐depth seismicityGeochemistry, Geophysics, Geosystems, 2005
- Vug waves: A mechanism for coupled rock deformation and fluid migrationGeochemistry, Geophysics, Geosystems, 2005
- Heat flow and bending-related faulting at subduction trenches: Case studies offshore of Nicaragua and Central ChileEarth and Planetary Science Letters, 2005
- Geophysical evidence for hydration of the crust and mantle of the Nazca plate during bending at the north Chile trenchGeology, 2004
- Bending-related faulting and mantle serpentinization at the Middle America trenchNature, 2003
- Fault patterns at outer trench wallsMarine Geophysical Research, 1991