Shear-wave velocity structure of the Chilean subduction zone (39-40 S) based on Rayleigh wave dispersion: evidence of fluid release and melts in the mantle beneath the Villarrica volcano::GFZpublic

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Shear-wave velocity structure of the Chilean subduction zone (39-40 S) based on Rayleigh wave dispersion: evidence of fluid release and melts in the mantle beneath the Villarrica volcano

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