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Could giant basin-forming impacts have killed Martian dynamo?
The observed strong remanent crustal magnetization at the surface of Mars suggests an active dynamo in the past and ceased to exist around early to middle Noachian era, estimated by examining remagnetization strengths in extant and buried impact basins. We investigate whether the Martian dynamo coul...
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| Gepubliceerd in: | Geophys Res Lett |
|---|---|
| Hoofdauteurs: | , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
BlackWell Publishing Ltd
2014
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4459199/ https://ncbi.nlm.nih.gov/pubmed/26074641 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2014GL061818 |
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