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The moon has no core dynamo magnetic field, but spacecraft detect numerous strong localized magnetic fields in the crust of the moon. Many of these magnetic anomalies are antipodal to large impact basins.
Scientists at Purdue University and the University of California, Santa Cruz, led by Brandon Johnson, Purdue associate professor of earth, atmospheric, and planetary sciences, ran impact The moon has no core dynamo magnetic field, but spacecraft detect numerous strong localized magnetic fields in the crust of the moon. Many of these magnetic anomalies are antipodal to large impact basins.
Scientists at Purdue University and the University of California, Santa Cruz, led by Brandon Johnson, Purdue associate professor of earth, atmospheric, and planetary sciences, ran impact simulations that showed that during oblique impact, ejected material piles up at the impact antipode.
This antipodal ejecta may be several-hundred meters thick. Much of this ejecta is impactor material, which may contain iron or other minerals that can become magnetized.
The authors found that this material is heated by the impact shockwave and remains warm enough to cool after it lands and records the moon's ancient magnetic field.
Using the strength of these anomalies and the calculated abundance of impactor material, they found that the moon's magnetic field had a strength of 40-73 uT at the time large impact basins were forming about 4 billion years ago.
Brief summary of methods
The team simulated basin-forming impacts to track material ejected far from the point of impact. They calculated that the trajectory of this ejecta determines where it lands with a focus on the distribution around the antipode of the impact (opposite side of the moon).
They also calculated the temperature and composition of this antipodal ejecta to determine if this antipodal ejecta can record the ancient lunar magnetic field.
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