RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES1002, doi:10.2205/2005ES000185, 2006

2005ES000185-fig05.html
Figure 5. Variation of the Siberian and European poles grouping (Ficherian precision parameter) as a function of the non-dipole coefficient values. In the cases of the non-dipole coefficients, when similar magnetic inclinations corresponded to different paleolatitudes (the use of inclinations gave ambiguous poles), when the values of the non-dipole coefficients were close to the boundary ones, calculations were made using the pole, located most closely to the neighboring exactly located pole, in the case of the close values of G2 and G3.

RJES

Citation: Veselovskiy, R. V., and V. E. Pavlov (2006), New paleomagnetic data for the Permian-Triassic Trap rocks of Siberia and the problem of a non-dipole geomagnetic field at the Paleozoic-Mesozoic boundary, Russ. J. Earth Sci., 8, ES1002, doi:10.2205/2005ES000185.

Copyright 2006 by the Russian Journal of Earth Sciences
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