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A silicate dynamo in the early Earth
The Earth’s magnetic field has operated for at least 3.4 billion years, yet how the ancient field was produced is still unknown. The core in the early Earth was surrounded by a molten silicate layer, a basal magma ocean that may have survived for more than one billion years. Here we use density func...
Uloženo v:
| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2020
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7042358/ https://ncbi.nlm.nih.gov/pubmed/32098945 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-14773-4 |
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