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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

Authors

Thorwart,  M.
External Organizations;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Dzierma,  Y.
External Organizations;
Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Lieser,  K.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Buhs,  H.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

Rabbel,  W.
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Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum;

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Citation

Thorwart, M., Dzierma, Y., Lieser, K., Buhs, H., Rabbel, W. (2015): 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. - In: Zellmer, G. F., Edmonds, M., Straub, S. M. (Eds.), The Role of Volatiles in the Genesis, Evolution and Eruption of Arc Magmas, (Geological Society special publication ; 410), 59-70.
https://doi.org/10.1144/SP410.9


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_1125890
Abstract
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