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...
Kaydedildi:
| Asıl Yazarlar: | , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Wiley
2021-06-01
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| Seri Bilgileri: | Geochemistry, Geophysics, Geosystems |
| Konular: | |
| Online Erişim: | https://doi.org/10.1029/2021GC009823 |
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