Evolving Subduction Zone Thermal Structure Drives Extensive Forearc Mantle Wedge Hydration

Abstract Hydration of the subduction zone forearc mantle wedge influences the downdip distribution of seismicity, the availability of fluids for arc magmatism, and Earth's long term water cycle. Reconstructions of present‐day subduction zone thermal structures using time‐invariant geodynamic models...

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Bibliografische Detailangaben

Hauptverfasser:	G. S. Epstein, C. B. Condit, R. K. Stoner, A. F. Holt, V. E. Guevara
Format:	Artigo
Sprache:	Inglês
Veröffentlicht:	Wiley 2024-08-01
Schriftenreihe:	AGU Advances
Schlagworte:	subduction serpentinization geodynamics volatile cycling metamorphic Petrology
Online-Zugang:	https://doi.org/10.1029/2023AV001121
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