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The ruthenium isotopic composition of the oceanic mantle
The approximately chondritic relative, and comparatively high absolute m antle abundances of the highly siderophile elem ents (HSE), suggest that their concentrations in the bulk silicate Earth were primarily established during a final ~0.5 to 1% of “late accretion” to the mantle, following the cess...
Gardado en:
| Publicado en: | Earth Planet Sci Lett |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
2017
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6448151/ https://ncbi.nlm.nih.gov/pubmed/30956285 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1016/j.epsl.2017.06.052 |
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