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

2005ES000182-fig15.html
Figure 15. Paleomagnetic poles: AT is the average Aisa-Taseeva pole; RDK is the Redkolesnaya Formation pole; HT1 and HT2 are the average poles for the respective components of the Mota, Irkutsk, Ust-Tagul, and Ostrovnaya rock formations; B1 and B2 are the average poles for the Late Vendian rocks in the southwest of the Cisbaikalia and in the east of the Sayan regions [Shatsillo et al., 5]; BT is the Biryusa-Tagul remagnetization pole; UR is the pole of the Urik remagnetization; GR is the pole of the Greben rock remagnetization (Angara region); BKN is the remagnetization pole of the Karagas rock series and the Nersa rock complex (Biryusa R. area) [Metelkin et al., 5]; Kir is the Kirschvink Tommotian Pole [Kirschvink and Rozanov, 1984]; KirCorr is the same pole corrected for the Vilyui Rift opening; V 2nd -kembry1tom is the pole for the boundary of the Nemakit-Daldynian and Tommotian beds of the Chekurov anticline (Lena R. lower course) [Pavlov et al., 2004]; kembry1tom is the Tommotian pole of the Olenek Rise [Pisarevsky et al., 1997]; kembry1toy is the Toyonian pole of the Olenek Rise [Gallet et al., 3]; kembry2amg+may is the Amga-Maya Pole of the Olenek Rise [Gallet et al., 2003]. The blue line shows the inferred Vendian-Cambrian trend of the apparent migration of the pole of the Siberian Platform.

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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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