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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| 主要な著者: | , , , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Wiley
2024-08-01
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| シリーズ: | AGU Advances |
| 主題: | |
| オンライン･アクセス: | https://doi.org/10.1029/2023AV001121 |
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