Cargando…
Delivery of carbon, nitrogen, and sulfur to the silicate Earth by a giant impact
Earth’s status as the only life-sustaining planet is a result of the timing and delivery mechanism of carbon (C), nitrogen (N), sulfur (S), and hydrogen (H). On the basis of their isotopic signatures, terrestrial volatiles are thought to have derived from carbonaceous chondrites, while the isotopic...
Autores principales: | Grewal, Damanveer S., Dasgupta, Rajdeep, Sun, Chenguang, Tsuno, Kyusei, Costin, Gelu |
---|---|
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/PMC6357864/ https://www.ncbi.nlm.nih.gov/pubmed/30746449 http://dx.doi.org/10.1126/sciadv.aau3669 |
Ejemplares similares
-
Behavior of light elements in iron-silicate-water-sulfur system during early Earth’s evolution
por: Iizuka-Oku, Riko, et al.
Publicado: (2021) -
The Speciation and Coordination of a Deep Earth Carbonate‐Silicate‐Metal Melt
por: Davis, A. H., et al.
Publicado: (2022) -
A silicate dynamo in the early Earth
por: Stixrude, Lars, et al.
Publicado: (2020) -
Reversal of carbonate-silicate cation exchange in cold slabs in Earth’s lower mantle
por: Lv, Mingda, et al.
Publicado: (2021) -
Crustal thickening and endogenic oxidation of magmatic sulfur
por: Tang, Ming, et al.
Publicado: (2020)