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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...

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Bibliografski detalji
Izdano u:Nat Commun
Glavni autori: Stixrude, Lars, Scipioni, Roberto, Desjarlais, Michael P.
Format: Artigo
Jezik:Inglês
Izdano: Nature Publishing Group UK 2020
Teme:
Online pristup: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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