The wet Nicaraguan slab

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The wet Nicaraguan slab

[1] Nicaraguan volcanoes show globally high concentrations of geochemical tracers from dehydration of subducting crust, which may reflect a slab with unusually high amounts of H2O. To test this possibility, we measure seismic velocities at the top of the subducted plate and compare them with predictions for hydrated mafic rocks. Regional seismic P waves for intraslab events at 100–150 km depth ...

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2003

ISSN: 0094-8276

DOI: 10.1029/2002gl015649