RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES2003, doi:10.2205/2005ES000182, 2006

Figure 12. The distribution of the
vectors of the high-temperature magnetization component in the
rocks of the Mota and Irkutsk formations (Urik R. area), in those
of the Ust-Tagul Formation (Biryusa R. and Tagul R. areas),
Ostrovnaya Formation (Angara R. area), and also of the
medium-temperature component of the Urik rock sequence. This
Figure also shows the summarized stereogram for the density
distribution of the axes of the respective high-temperature
magnetization components. The stereograms are plotted in the
stratigraphic system of the coordinates. The solid circles show
the projections to the lower hemisphere, the open ones, to the
upper. All axes of the density stereogram face the lower
hemisphere.

Citation: Shatsillo, A. V., V. E. Pavlov, and A. N. Didenko (2006), Paleomagnetism of Vendian rocks in the southwest of the Siberian Platform, Russ. J. Earth Sci., 8, ES2003, doi:10.2205/2005ES000182.
Copyright 2006 by the Russian Journal of Earth Sciences
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