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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...
| Autores principales: | , , , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2021
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| Materias: | |
| 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 |