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

Figure 4. The distances
(gamma angles) between the Siberian and European average poles as
a function of the values of the non-dipole component
contributions. The stepwise pattern of the marginal parts of the
curves was controlled by the discrete values of the
G2 and
G3
components (1%) used in the calculations.

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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