Cargando…
Volatile element depletion of the Moon—The roles of precursors, post-impact disk dynamics, and core formation
The compositional and isotopic similarity of Earth’s primitive upper mantle (PUM) and the Moon supports the derivation of the Moon from proto-Earth, but the Moon’s inventory of volatile lithophile elements—Na, K, Rb, and Cs—is lower than Earth’s PUM by factors of 4 to 5. The abundances of 14 other v...
Autor principal: | Righter, K. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Association for the Advancement of Science
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6357731/ https://www.ncbi.nlm.nih.gov/pubmed/30746461 http://dx.doi.org/10.1126/sciadv.aau7658 |
Ejemplares similares
-
Depletion of potassium and sodium in mantles of Mars, Moon and Vesta by core formation
por: Steenstra, E. S., et al.
Publicado: (2018) -
The origin of volatile elements in the Earth–Moon system
por: Borg, Lars E., et al.
Publicado: (2022) -
Extensive volatile loss during formation and differentiation of the Moon
por: Kato, Chizu, et al.
Publicado: (2015) -
Isotopic evolution of the protoplanetary disk and the building blocks of Earth and Moon
por: Schiller, Martin, et al.
Publicado: (2018) -
Gallium isotopic evidence for extensive volatile loss from the Moon during its formation
por: Kato, Chizu, et al.
Publicado: (2017)