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Persistence and origin of the lunar core dynamo

机译:Persistence and origin of the lunar core dynamo

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摘要

The lifetime of the ancient lunar core dynamo has implications for its power source and the mechanismoffield generation.Here,we report analyses of two 3.56-Gy-old mare basalts demonstrating that they were magnetized in a stable and surprisingly intense dynamo magnetic field of at least~13 μT. These data extend the known lifetime of the lunar dynamo by ~160 My and indicate that the field was likely continuously active until well after the final large basin-forming impact. This likely excludes impact-driven changes in rotation rate as the source of the dynamo at this time in lunar history. Rather, our results require a persistent power source like precession of the lunar mantle or a compositional convection dynamo.

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