Covariation of Slab Tracers, Volatiles, and Oxidation During Subduction Initiation

Abstract Subduction‐related lavas have higher Fe3+/∑Fe than midocean ridge basalts (MORB). Hypotheses for this offset include imprint from subducting slabs and differentiation in thickened crust. These ideas are readily tested through examination of the time‐dependent evolution of slab‐derived signa...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Maryjo Brounce, Mark K. Reagan, Katherine A. Kelley, Elizabeth Cottrell, Kenji Shimizu, Renat Almeev
Format: Article
Language:English
Published: Wiley 2021-06-01
Subjects:
Online Access:https://doi.org/10.1029/2021GC009823