NASA NTRS · 20050170997
Evidence for a Second Martian Dynamo from Electron Reflection Magnetometry
Abstract
Present-day Mars does not possess an active core dynamo and associated global magnetic field. However, the discovery of intensely magnetized crust in Mars Southern hemisphere implies that a Martian dynamo has existed in the past. Resolving the history of the Martian core dynamo is important for understanding the evolution of the planet's interior. Moreover, because the global magnetic field provided by an active dynamo can shield the atmosphere from erosion by the solar wind, it may have influenced past Martian climate. Additional information is included in the original extended abstract.
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Lillis, R. J., Manga, M., Mitchell, D. L., Lin, R. P., Acuna, M. H.. 2005-01-01. Evidence for a Second Martian Dynamo from Electron Reflection Magnetometry. https://ntrs.nasa.gov/citations/20050170997
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