Abstract
Both the magnitude and direction of the palaeomagnetic field have been determined during a field reversal. The results indicate that the geomagnetic field was large and stable when the magnetic pole was close to the equator. Copyright © 1975, Wiley Blackwell. All rights reserved
Cite
CITATION STYLE
APA
Shaw, J. (1975). Strong Geomagnetic Fields during a single Icelandic Polarity Transition. Geophysical Journal of the Royal Astronomical Society, 40(3), 345–350. https://doi.org/10.1111/j.1365-246X.1975.tb04136.x
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