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Hydrous Regions of the Mantle Transition Zone Lie Beneath Areas of Continental Intraplate Volcanism

Abstract Great volumes of water are carried downward into the mantle transition zone (MTZ, 410–670 km depth) by subducting slabs. If this water is later drawn upward, the resulting mantle melting may generate continental intraplate volcanism (IPV). Despite water's importance, its amount and spatial...

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Principais autores: Helene Wang, Valentina Magni, Clinton P. Conrad, Mathew Domeier
Formato: Artigo
Idioma:Inglês
Publicado em: Wiley 2025-03-01
coleção:Geochemistry, Geophysics, Geosystems
Assuntos:
mantle dynamics
intraplate volcanism
mantle hydration
regassing
mantle transition zone
subduction
Acesso em linha:https://doi.org/10.1029/2024GC011901
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