Asteroid material deposited during large impacts record the moon’s ancient magnetic field


When something hits the moon at an oblique angle, ejected material — including pieces of the impactor, which may contain iron ore or other magnetic metals — accumulates on the opposite side of the moon. This accumulation, which may be several-hundred meters thick, records the strength of the moon’s magnetic field at the time of impact, allowing researchers a glimpse into the moon’s magnetic past. Credit: Purdue University image/Shigeru Wakita

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 μT at the time large impact basins were forming about 4 billion years ago.

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. 

Credit: Purdue University

Brandon Johnson, associate professor in Purdue University’s Department of Earth, Atmospheric, and Planetary Sciences, is an expert on impact cratering, one of the most pervasive geologic processes in the solar system. First author is Shigeru Wakita, Johnson’s former postdoctoral researcher.

The research was published in Nature Communications.

Was the moon magnetized by impact plasmas?

More information:
S. Wakita et al, Impactor material records the ancient lunar magnetic field in antipodal anomalies, Nature Communications (2021). DOI: 10.1038/s41467-021-26860-1

Provided by
Purdue University

Asteroid material deposited during large impacts record the moon’s ancient magnetic field (2021, November 30)
retrieved 30 November 2021

This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no
part may be reproduced without the written permission. The content is provided for information purposes only.



Read original article here

Denial of responsibility! Samachar Central is an automatic aggregator of the all world’s media. In each content, the hyperlink to the primary source is specified. All trademarks belong to their rightful owners, all materials to their authors. If you are the owner of the content and do not want us to publish your materials, please contact us by email – [email protected]. The content will be deleted within 24 hours.

Leave a comment