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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...

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Principais autores: Maryjo Brounce, Mark K. Reagan, Katherine A. Kelley, Elizabeth Cottrell, Kenji Shimizu, Renat Almeev
Format: Artigo
Jezik:Inglês
Izdano: Wiley 2021-06-01
Serija:Geochemistry, Geophysics, Geosystems
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Online dostop:https://doi.org/10.1029/2021GC009823
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