RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES1004, doi:10.2205/2006ES000191, 2006

Figure 7. The distribution of the magnitudes of the geomagnetic
field direction variations (Sp)
as a function of the distance to the center of
the Siberian traps, based on the whole
collection of the data. The rhombs show the
lavas, the circles show the sediments, the +
symbols, the intrusive rocks, the red symbols
showing the data of high paleomagnetic
reliability, the green ones, the intermediate
reliability, and the black ones, the low
reliability.

Citation: Pechersky, D. M. (2006), Geomagnetic field in the vicinity of the Paleozoic-Mesozoic boundary and the Siberian superplume, Russ. J. Earth Sci., 8, ES1004, doi:10.2205/2006ES000191.
Copyright 2006 by the Russian Journal of Earth Sciences
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