Fluid‐Mediated Mass Transfer Between Mafic and Ultramafic Rocks in Subduction Zones

Fluid‐Mediated Mass Transfer Between Mafic and Ultramafic Rocks in Subduction Zones

Abstract Metasomatic reaction zones between mafic and ultramafic rocks exhumed from subduction zones provide a window into mass‐transfer processes at high pressure. However, accurate interpretation of the rock record requires distinguishing high‐pressure metasomatic processes from inherited oceanic...

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Bibliographic Details
Main Authors: E. A. Codillo, F. Klein, B. Dragovic, H. R. Marschall, E. Baxter, M. Scambelluri, E. Schwarzenbach‬
Format: Article
Language:English
Published: Wiley 2022-08-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
fluid‐rock interactions
magnesium metasomatism
subduction zones
Voltri Massif
Online Access:https://doi.org/10.1029/2021GC010206

Internet

https://doi.org/10.1029/2021GC010206

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