The Mantle Fe3+/ΣFe Ratio Has Doubled Since the Early Archean
Abstract How mantle redox state developed, particularly the mantle source associated with mid-ocean ridge-like settings, remains a subject of ongoing debate. Here, we employ thermodynamic-thermomechanical numerical simulations to explore the redox properties of melts formed under mid-ocean ridge-lik...
Kaydedildi:
| Asıl Yazarlar: | , , , , |
|---|---|
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2026-01-01
|
| Seri Bilgileri: | Nature Communications |
| Online Erişim: | https://doi.org/10.1038/s41467-025-66969-1 |
| Etiketler: |
Etiket eklenmemiş, İlk siz ekleyin!
|