How the geomagnetic field vector reverses polarity

Details How the geomagnetic field vector reverses polarity How the geomagnetic field vector reverses polarity

Jul 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985natur.316..230p&link_type=abstract

Nature (ISSN 0028-0836), vol. 316, July 18, 1985, p. 230-234.

Mathematics

70

Geomagnetism, Magnetic Field Inversions, Magnetic Poles, Paleomagnetism, Polarity, Geomagnetic Pulsations, Magnetic Dipoles, Vectors (Mathematics)

Scientific paper

A highly detailed record of both the direction and intensity of the earth's magnetic field as it reverses has been obtained from a Miocene volcanic sequence. The transitional field is low in intensity and is typically nonaxisymmetric. Geomagnetic impulses corresponding to astonishingly high rates of change of the field sometimes occur, suggesting that liquid velocity within the earth's core increases during geomagnetic reversals.

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