Anomalous geomagnetic variations on the island of South Georgia

Observations of geomagnetic variation fields on South Georgia, in the Scotia Sea, have revealed an unusual polarisation anomaly in the horizontal components, whose characteristics cannot be accounted for by an ocean-edge effect model. In addition, vertical field transfer functions have been calculat...

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Bibliographic Details
Published in:Journal of geomagnetism and geoelectricity
Main Author: Beamish, David
Format: Article in Journal/Newspaper
Language:English
Published: Society of Geomagnetism and Earth, Planetary and Space Sciences 1982
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/516901/
https://nora.nerc.ac.uk/id/eprint/516901/1/NORA_Beamish_1982_JofG%26G.pdf
https://doi.org/10.5636/jgg.34.479
Description
Summary:Observations of geomagnetic variation fields on South Georgia, in the Scotia Sea, have revealed an unusual polarisation anomaly in the horizontal components, whose characteristics cannot be accounted for by an ocean-edge effect model. In addition, vertical field transfer functions have been calculated in the period range 10-10000 s. Although the data obtained from only one station allows only a limited analysis, it is suggested that the anomalous geomagnetic response on South Georgia can be accounted for by lithospheric conductivity contrasts between the Scotia and South American Plates.