Palaeointensity determinations on Apollo 11, 16 and 17 rocks have indicated that 3.9 - 4.0 AE ago the strength of the surface lunar magnetic field was about 1.3 Oe while there is evidence from younger rocks that a field of about one quarter of this value was present at a later time (3.6 AE). (Author)
The Intensity of the Ancient Lunar Field from Magnetic Studies on Lunar Samples
1974
13 pages
Report
No indication
English
Micropaleontological studies of lunar samples
NTRS | 1971
|Magnetic studies of lunar samples - Breccia and fines
NTRS | 1970
|