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

2005ES000185-fig07.html
Figure 7. Example of an error in determining the paleolatitude position where the geomagnetic field differed from the dipole one. The red curves show the errors obtained for different inclination shallowing factors. The blue curve shows an error for the contribution of the octupolar component measuring - 10% to the magnetic field of the Earth.

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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