RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES3003, doi:10.2205/2005ES000175, 2005

Figure 5. The example of the relative paleointensity variation obtained after studying the
magnetization of the rocks from 12 ocean-floor core samples for the time interval of 50 thousand years.
The DIP2 paleointensity decline corresponds to the Matuyama/Brunes boundary, the DIP1 reflecting the
triggering mechanism of the reversal, as follows from our interpretation of Figure 6 from
[Hartl and Tauxe, 1996].

Citation: Gurarii, G. Z. (2005), Geomagnetic field reversals: Main results and basic problems, Russ. J. Earth Sci., 7, ES3003, doi:10.2205/2005ES000175.
Copyright 2005 by the Russian Journal of Earth Sciences
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