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Selenium isotopes as tracers of a late volatile contribution to Earth from the outer Solar System
The origin of Earth’s volatiles has been attributed to a late addition of meteoritic material after core-mantle differentiation. The nature and consequences of this 'late veneer' are debated, but may be traced by isotopes of the highly siderophile, or iron-loving, and volatile element sele...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6726489/ https://www.ncbi.nlm.nih.gov/pubmed/31485262 http://dx.doi.org/10.1038/s41561-019-0414-7 |