Abstract
The discovery that rocks of the lunar crust possess remanent magnetism is a surprising result in view of the fact that the present Moon does not exhibit a magnetic field, nor was there once evidence of an iron core in which one could be generated. This review looks at the concept of lunar palaeomagnetism and discusses its implications for lunar science as a whole.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
