Early Cambrian renewal of the geodynamo and the origin of inner core structure
New single crystal paleointensity data show that the geomagnetic field was renewed in the early Cambrian after near collapse in the Ediacaran Period. This implies that the innermost/outermost structure of the inner core formed 450 million yrs. ago.
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| Principais autores: | , , , , , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Portfolio
2022-07-01
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| coleção: | Nature Communications |
| Acesso em linha: | https://doi.org/10.1038/s41467-022-31677-7 |
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