Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
Summary: Previous subduction thermal models are inconsistent with the values of forearc heat flow (50–140 mW/m2) and global P‒T conditions of exhumed rocks, both suggesting a shallow environment 200–300°C warmer than model predictions. Here, we revaluate these problems in Kuril-Kamchatka using 3D th...
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| Autors principals: | , , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Elsevier
2023-08-01
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| Col·lecció: | iScience |
| Matèries: | |
| Accés en línia: | http://www.sciencedirect.com/science/article/pii/S2589004223013652 |
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