Sharp fluctuation of the direction of the geomagnetic field (excurse) detected during paleomagnetic studies in the Tashkent region

Details Sharp fluctuation of the direction of the geomagnetic field (excurse) detected during paleomagnetic studies in the Tashkent region Sharp fluctuation of the direction of the geomagnetic field (excurse) detected during paleomagnetic studies in the Tashkent region

Feb 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992ge%26ae..32..132p&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 32, no. 1, Jan.-Feb. 1992, p. 132-139. In Russian.

Physics

Geomagnetism, Magnetic Field Inversions, Paleomagnetism, Ferromagnetism, Magnetic Anomalies, Magnetic Fields, Spatial Distribution

Scientific paper

A sharp fluctuation of the geomagnetic-field direction detected during a
paleomagnetic investigation in the Tashkent region is identified as the
Kargapolovo excurse, which fits in the scatter of age estimates. The
duration of the excurse is estimated to be about 4000 years.

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