Melting of subducted sediments reconciles geophysical images of subduction zones

Here, the authors identify that magnetotelluric conductive anomalies commonly observed on the trenchward-side of volcanic arcs in subduction zones can be explained by subducted sediments. High-pressure experiments show that these sediment melts will react with the overlying mantle wedge to produce e...

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Auteurs principaux: M. W. Förster, K. Selway
Format: article
Langue:EN
Publié: Nature Portfolio 2021
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Accès en ligne:https://doaj.org/article/86e1e86e7dab4aec9259af27d6754f95
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