Earth's magnetic field first appeared within a specific timeframe after planetary accretion
Geological evidence from ancient zircons indicates that Earth's magnetic field emerged at least 4.2 billion years ago, placing its origin within a specific early timeframe following planetary accretion.
The retrieved literature consistently supports the existence of an early Hadean geodynamo dating back at least 4.2 billion years, as documented through paleomagnetic analysis of zircons. This demonstrates that Earth's magnetic field appeared within a specific, relatively short timeframe after planetary accretion.
Tarduno JA, Cottrell RD, Bono RK, Oda H, Davis WJ, Fayek M, Erve OV', Nimmo F, Huang W, Thern ER, Fearn S, Mitra G, Smirnov AV, Blackman EG. Paleomagnetism indicates that primary magnetite in zircon records a strong Hadean geodynamo.. 2020. https://doi.org/10.1073/pnas.1916553117
Paper 5 shows via zircon paleomagnetism that Earth's magnetic field existed at least 4.2 billion years ago, soon after planetary formation and the giant impact.
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Tarduno JA, Tarduno JA, Zhou T, Huang W, Jodder J. Earth's magnetic field and its relationship to the origin of life, evolution and planetary habitability.. 2025. https://doi.org/10.1093/nsr/nwaf082
Paper 11 confirms that the geomagnetic field was established at least 4.2 billion years ago, providing an early Hadean origin that shielded the planet.
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