Long-term reduced lunar mantle revealed by Chang’e-5 basalt
Abstract The redox state of a planetary mantle affects its thermal evolution. The redox evolution of lunar mantle, however, remains unclear due to limited oxygen fugacity (fO2) constraints from young lunar samples. Here, we report vanadium (V) oxybarometers on olivine and spinel conducted on 27 Chan...
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| Autori principali: | , , , , , , , , , , , , , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Portfolio
2024-09-01
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| Serie: | Nature Communications |
| Accesso online: | https://doi.org/10.1038/s41467-024-52710-x |
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