Physics
Scientific paper
Feb 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992geoji.108..613p&link_type=abstract
Geophysical Journal International, Vol. 108, No. 2, p. 613 - 620
Physics
23
Scientific paper
The authors present a compilation of palaeointensity data obtained by the Thellier method from magnetic rocks up to 3.5 Gyr old. No apparent very long-term variation occurs from present to Early Precambrian. The overall data are compatible with a gravitationally powered dynamo model in which the inner core is some 4.0 Gyr old. However, palaeointensity data are still too incomplete to dismiss the possibility of a more complex field history with a geodynamo first thermally driven then gravitationally powered. Despite the limited number of data currently available, large differences in the dipole field moment are clearly documented with a time-scale of the order of 50-100 Myr. The changes in intensity can be due to repetitive instabilities of the thermal boundary layer at the base of the mantle.
Perrin Marshall
Prévot Michel
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