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Geomagnetic spikes on the core-mantle boundary
Extreme variations of Earth's magnetic field occurred in the Levant region around 1000 BC, when the field intensity rapidly rose and fell by a factor of 2. No coherent link currently exists between this intensity spike and the global field produced by the core geodynamo. Here we show that the L...
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| Udgivet i: | Nat Commun |
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| Main Authors: | , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Nature Publishing Group
2017
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5459996/ https://ncbi.nlm.nih.gov/pubmed/28555646 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms15593 |
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