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Fluid-rock interaction processes in ancient subduction zones evidenced by the high-pressure–low-temperature Acatlán complex, Mexico

Abstract Subduction zones play a crucial role in controlling interactions between the oceanic crust and mantle, generating fluid and hydrous melt, and facilitating subsequent volatile and mass transfer to mantle depths. In the Acatlán Complex, Mexico, trace elements, Sr–Nd isotopes, petrological mod...

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Principais autores: Fabián Gutiérrez-Aguilar, Sofía Jiménez-Barranco, Peter Schaaf, Alfredo Victoria-Morales
Formato: Artigo
Idioma:Inglês
Publicado: Nature Portfolio 2025-04-01
Series:Scientific Reports
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Acceso en liña:https://doi.org/10.1038/s41598-025-93279-9
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