Other
Scientific paper
Feb 1978
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978sci...199..771r&link_type=abstract
Science, vol. 199, Feb. 17, 1978, p. 771-773.
Other
13
Dynamo Theory, Lunar Core, Lunar Evolution, Lunar Magnetic Fields, Paleomagnetism, Heat Sources, Iron, Lunar Composition, Planetary Structure, Moon, Origin, Magnetic Fields, Paleomagnetism, Iron, Thermal History, Remanent Magnetization, Core
Scientific paper
Lunar paleomagnetism provides evidence for the existence of an ancient lunar magnetic field generated in an iron core. Paleointensity experiments give a surface field of 1.3 gauss, 4.0 x 10 to the 9th years ago, subsequently decreasing exponentially. Thermodynamic arguments give a minimum value of the heat source in the core at that time: known sources, radioactive and other, are quantitatively implausible, and it is suggested that superheavy elements were present in the early moon.
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