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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...

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Detalles Bibliográficos
Autores principales: Lantink, Margriet L., Davies, Joshua H. F. L., Ovtcharova, Maria, Hilgen, Frederik J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2022
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

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