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...

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Detalles Bibliográficos
Autores principales: Zhu, Weiling, Ji, Yingfeng, Liu, Lijun, Qu, Rui, Zhu, Ye, Xie, Chaodi, Ding, Lin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2023
Materias:
Article
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

Internet

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

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