Oxygen isotope shifts reveal fluid-fluxed melting in continental anatexis

Abstract Fluid-flux melting is increasingly recognised as a key mechanism for continental crust growth and recycling, but the abundance and sources of the external fluids involved in this process are typically uncertain. Here we use zircon and garnet oxygen isotope data, geochronology, and petrologi...

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Bibliographic Details
Main Authors: Silvia Volante, Amaury Pourteau, Zheng-Xiang Li, William J. Collins, Luc S. Doucet, Hugo K. H. Olierook, Laure Martin, Matthijs A. Smit
Format: Article
Language:English
Published: Nature Portfolio 2025-04-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02250-z
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