Redox evolutions of planetary mantle reservoirs constrained by titanium isotopes
Abstract The oxygen fugacity (hereafter referred as fO2) of terrestrial planets is key in defining the outcome of planetary-scale differentiation and the planets’ potential habitability. Reconstructing the initial fO2 records in the mantle right after core formation for terrestrial planets remain ch...
| الحاوية / القاعدة: | Communications Earth & Environment |
|---|---|
| المؤلفون الرئيسيون: | , , , , , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Nature Portfolio
2025-09-01
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| الوصول للمادة أونلاين: | https://doi.org/10.1038/s43247-025-02692-5 |