Cargando…
Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust
Oxygen fugacity (ƒO(2)) is an intensive variable implicated in a range of processes that have shaped the Earth system, but there is controversy on the timing and rate of oxidation of the uppermost convecting mantle to its present ƒO(2) around the fayalite-magnetite-quartz oxygen buffer. Here, we rep...
| Autores principales: | , , , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
|
| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6934757/ https://www.ncbi.nlm.nih.gov/pubmed/31882582 http://dx.doi.org/10.1038/s41598-019-55743-1 |