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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Bibliographic Details
Main Authors: Fabián Gutiérrez-Aguilar, Sofía Jiménez-Barranco, Peter Schaaf, Alfredo Victoria-Morales
Format: Article
Language:English
Published: Nature Portfolio 2025-04-01
Series:Scientific Reports
Subjects:
Online Access:https://doi.org/10.1038/s41598-025-93279-9
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