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

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.

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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