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

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 -
1tom 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];
1tom is the Tommotian pole of the Olenek Rise [Pisarevsky et al.,
1997];
1toy is the
Toyonian pole of the Olenek Rise [Gallet et al.,
3];
2amg+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.

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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