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Siderophile element constraints on the origin of the Moon
Discovery of small enrichments in (182)W/(184)W in some Archaean rocks, relative to modern mantle, suggests both exogeneous and endogenous modifications to highly siderophile element (HSE) and moderately siderophile element abundances in the terrestrial mantle. Collectively, these isotopic enrichmen...
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
The Royal Society Publishing
2014
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| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4128271/ https://ncbi.nlm.nih.gov/pubmed/25114313 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2013.0258 |
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