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Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago
The long-term history of the Earth–Moon system as reconstructed from the geological record remains unclear when based on fossil growth bands and tidal laminations. A possibly more robust method is provided by the sedimentary record of Milankovitch cycles (climatic precession, obliquity, and orbital...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
National Academy of Sciences
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9546617/ https://www.ncbi.nlm.nih.gov/pubmed/36161904 http://dx.doi.org/10.1073/pnas.2117146119 |