Longitudinal confinement of geomagnetic reversal paths as a possible sedimentary artefact

Physics

Scientific paper

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Geomagnetism, Magnetic Field Inversions, Magnetic Poles, Sediments, Asia, Australia, Paleomagnetism, Zonal Harmonics

Scientific paper

It is shown here that longitudinal confinement of virtual geomagnetic
poles can arise from the smoothing of nonantipodal stable directions
before and after a geomagnetic reversal, because of the filtering effect
of the remanence acquisition process in sediments. The origin of this
nonantipodality is still uncertain.

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