RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 9, ES1002, doi:10.2205/2007ES000221, 2007

Figure 1. Isotopic-geochemical ratios variations. Pechishchi section.
1 - sandstones, 2 - siltstones, 3 - siltstones and sandstones,
4 - siltstones and clays, 5 - clays, 6 - limestones, 7 - clayer limestones,
8 - sandy limestones, 9 - dolomites, 10 - clayer dolomites, 11 - marls,
12 - coal, 13 - hypsum, 14 - coarse grains, 15 - oolites, 16 - reefs remains,
17 - caverns, 18 - carbonate inclusions, 19 - SiO2, 20 - celestine,
21 - foraminifers, 22 - marine ostracodes, 23 - non-marine ostracodes,
24 - conchostracans, 25 - gastropods, 26 - marine bivalves,
27 - non-marine bivalves, 28 - nautiloidei, 29 - inarticulate brachiopods,
30 - articulate brachiopods, 31 - bryozoans, 32 - crinoids, 33 - fish remains,
34 - finds of fish, 35 - tetrapods, 36 - conodonts, 37 - fauna textures,
38 - plant remains, 39 - charophytes, 40 - miospores.
Noinsky's cycles components: F - faunistic carbonate beds, E - evaporites,
C -clays and marls.

Citation: Nurgalieva, N. G., V. A. Ponomarchuk, and D. K. Nurgaliev (2007), Strontium isotope stratigraphy: Possible applications for age estimation and global correlation of Late Permian carbonates of the Pechishchi type section, Volga River, Russ. J. Earth Sci., 9, ES1002, doi:10.2205/2007ES000221.
Copyright 2007 by the Russian Journal of Earth Sciences
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