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A two-billion-year history for the lunar dynamo
Magnetic studies of lunar rocks indicate that the Moon generated a core dynamo with surface field intensities of ~20 to 110 μT between at least 4.25 and 3.56 billion years ago (Ga). The field subsequently declined to <~4 μT by 3.19 Ga, but it has been unclear whether the dynamo had terminated by...
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| Publicado no: | Sci Adv |
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| Main Authors: | , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Association for the Advancement of Science
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5550224/ https://ncbi.nlm.nih.gov/pubmed/28808679 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1700207 |
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