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Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures
Previous subduction thermal models are inconsistent with the values of forearc heat flow (50–140 mW/m(2)) 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 thermomec...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Elsevier
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10382886/ https://www.ncbi.nlm.nih.gov/pubmed/37520704 http://dx.doi.org/10.1016/j.isci.2023.107288 |