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

2005ES000185-fig04.html
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.

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
Powered by TeXWeb (Win32, v.2.0).