Silurian sediments of the extreme southwest of Tuva
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Abstract
In the extreme southwest of Tuva, the Silurian sediments are composed of small isolated mulds. The largest of these is the Mugur syncline, and two other small folds are located in the area of the Ordovician Kargin syncline...
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References
- Amantov V. A. A brief sketch of the stratigraphy of the Silurian sediments of the Valley of the Great Lakes in comparison with the Silurian of the Tuva Trough. Proc. VSEGEI, new series, No. 58, 1961.
- Bartseva M. N., Potapova M. S. Altai and Kalba. In the book: Silurian System. Nedra, 1965.
- Vladimirskaya E. V., Chekhovich V. D. Biostratigraphy of the Silurian of Tuva. Geology and Geophysics, No. 4, 1969.
- Luvsandanzan B. Stratigraphy of the Paleozoic of the Mongolian Altai. In the book: Stratigraphy and Tectonics of the Mongolian People’s Republic. Nauka, 1970.
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