Oxygen isotopic evidence for accretion of Earth’s water before a high-energy Moon-forming giant impact

The Earth-Moon system likely formed as a result of a collision between two large planetary objects. Debate about their relative masses, the impact energy involved, and the extent of isotopic homogenization continues. We present the results of a high-precision oxygen isotope study of an extensive sui...

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Detalles Bibliográficos
Autores principales: Greenwood, Richard C., Barrat, Jean-Alix, Miller, Martin F., Anand, Mahesh, Dauphas, Nicolas, Franchi, Ian A., Sillard, Patrick, Starkey, Natalie A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2018
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5873841/
https://www.ncbi.nlm.nih.gov/pubmed/29600271
http://dx.doi.org/10.1126/sciadv.aao5928

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5873841/
https://www.ncbi.nlm.nih.gov/pubmed/29600271
http://dx.doi.org/10.1126/sciadv.aao5928

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