Variations of the direction and magnitude of the geomagnetic field in the Phanerozoic era

Details Variations of the direction and magnitude of the geomagnetic field in the Phanerozoic era Variations of the direction and magnitude of the geomagnetic field in the Phanerozoic era

Oct 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988ge%26ae..28..820p&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 28, Sept.-Oct. 1988, p. 820-824. In Russian.

Physics

Geomagnetism, Magnetic Field Configurations, Paleomagnetism, Sedimentary Rocks, Standard Deviation, Continental Drift, Spectral Correlation

Scientific paper

The paper summarizes data on the standard deviation of paleomagnetic
directions of sedimentary rocks reflecting the sum amplitude of
variations of the geomagnetic field and the inversion frequency.
Smoothed field variation curves are constructed for the Phanerozoic with
a smoothing interval of 30 million years and a step of 10 million years.

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