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 mo...

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发表在:	AGU Advances
Main Authors:	G. S. Epstein, C. B. Condit, R. K. Stoner, A. F. Holt, V. E. Guevara
格式:	文件
语言:	英语
出版:	Wiley 2024-08-01
主题:	subduction serpentinization geodynamics volatile cycling metamorphic Petrology
在线阅读:	https://doi.org/10.1029/2023AV001121