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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...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Prif Awduron: Maryjo Brounce, Mark K. Reagan, Katherine A. Kelley, Elizabeth Cottrell, Kenji Shimizu, Renat Almeev
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Wiley 2021-06-01
Cyfres:Geochemistry, Geophysics, Geosystems
Pynciau:
Mynediad Ar-lein:https://doi.org/10.1029/2021GC009823
Tagiau: Ychwanegu Tag
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