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

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.

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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