Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites

Fractionation effects related to evaporation and condensation had a major impact on the current elemental and isotopic composition of the Solar System. Although isotopic fractionation of moderately volatile elements has been observed in tektites due to impact heating, the exact nature of the process...

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Detalles Bibliográficos
Autores principales: Chernonozhkin, S. M., González de Vega, C., Artemieva, N., Soens, B., Belza, J., Bolea-Fernandez, E., Van Ginneken, M., Glass, B. P., Folco, L., Genge, M. J., Claeys, Ph., Vanhaecke, F., Goderis, S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8458397/
https://www.ncbi.nlm.nih.gov/pubmed/34552090
http://dx.doi.org/10.1038/s41467-021-25819-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8458397/
https://www.ncbi.nlm.nih.gov/pubmed/34552090
http://dx.doi.org/10.1038/s41467-021-25819-6

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