RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES5001, doi:10.2205/2008ES000302, 2008

2008ES000302-fig06.html

Figure 6. Correlation of sections of the Kuragan, Guberlya, and Baulus formations in the Sakmara and eastern Sakmara-Voznesenka zones: 1 - carbonaceous shales and cherts; 2 - arkoses; 3 - siltstones, argillites, and arkoses; 4 - tuffaceous sandstones and siltstones; 5 - tuffites of mixed composition; 6 - tuffaceous sandstones and gravelstones; 7 - variegated siliceous tephroids; 8 - grey siliceous tephroids; 9 - basalts; 10 - andesites; 11 - rhyolites and dacites; 12 - rhyolite and dacite tuffs; 13 - massive sulfide ores; 14 - points of conodont and other organic remains localities and their numbers. Redeposited conodonts are recorded at Point 2ast.


RJES

Citation: Dubinina, S. V., and A. V. Ryazantsev (2008), Conodont stratigraphy and correlation of the Ordovician volcanogenic and volcanogenic sedimentary sequences in the South Urals, Russ. J. Earth Sci., 10, ES5001, doi:10.2205/2008ES000302.

Copyright 2008 by the Russian Journal of Earth Sciences
Powered by TeXWeb (Win32, v.2.0).