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

Figure 2. The schematic
geological structure of the Yenisey Ridge study area. Legend:
1 - Neogene, 2 - Permian-Triassic traps, 3 - Carboniferous and
Permian rocks, 4 - Middle-Upper Cambrian (Upper Lena Formation),
5 - Lower Cambrian, 6 - Upper Riphean(?) to Vendian rocks
(Taseeva Series: Redkolesnaya and Ostrovnaya formations),
7 - pre-Vendian rocks, 8 - faults; 9 - objects of study:
(1) the Irkineeva R. area: the rocks of the Redkolesnaya
Formation; (2) the left bank of the Angara R. below the Man'zya
Settlement: the rocks of the Chistyakova and Moshakova formations,
(3) the right bank of the Angara R. from the Gremyachiy Creek to
the Greben Cliff: the Chistyakova, Moshakova, Redkolesnaya, and
Ostrovnaya formations, (4) the right bank of the Taseeva R. below
the mouth of the Usolka River: the Alesha Formation, and (5) the
right bank of the Taseeva R. in the area of the Dyrovatyi Cliff:
the Kliminskaya Formation.

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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