Intensity and origin of the ancient lunar magnetic field

Author:

Abstract

There is now strong evidence that the Moon possessed a magnetic field between 4000 and 3200 Ma ago. The evidence for and origin of this field are discussed, and determinations of its intensity described. It is tentatively concluded that the field decreased from an initial intensity of about 1 G (10-4 T) during the above time interval, and the implications of the initial intensity and its decay for the origin of the field are discussed.

Publisher

The Royal Society

Subject

General Engineering

Cited by 12 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. The formation of the lunar core;Geochimica et Cosmochimica Acta;1996-04

2. The early magnetic field and primeval satellite system of the Moon: clues to planetary formation;Philosophical Transactions of the Royal Society of London. Series A: Physical and Engineering Sciences;1994-11-15

3. Some Reflections on Solid State Convection in the Mantles of the Earth, Moon and Terrestrial Planets;Flow and Creep in the Solar System: Observations, Modeling and Theory;1993

4. The primaeval lunar magnetic field: Its relevance to the interpretation of planetary fields;Advances in Space Research;1992-08

5. Remanent magnetic properties of unbrecciated eucrites;Earth and Planetary Science Letters;1991-10

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