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

2005ES000182-fig12.html
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.

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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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