Geology of the folding fundament of the Tobola river highways district (northwestern part of the Turgai trough).
Abstract
The folded formations developed in the northwestern part of the Turgai Trough appear on the day surface only in the valleys of the Tobol River and its largest tributaries, where they were studied by Meglitsky and Antipov, A. A. Krasnopolsky, A. N. Geisler (1929), D. S. Steinberg (1929), A. P. Zotov (1935) ( A. G. Behr, G. A. Sokolov (1934), E. A. Ushakova (1932), K. I. Dvortsova (1937-1940), F. N. Ruvikova (1937-1940), and F. N. Ruvikova (1937-1940). G. Ber, G. A. Sokolov (1934), E. A. Ushakova (1932), K. I. Dvortsova (1937-1940), F. N. Rukavishnikov (1938), A. P. Krotov (1943), E. I. Klevtsov (1946-1947), N. N. Pikhtovnikova (1946), E. A. Mazina and other researchers. Huge areas of watersheds remained practically unexplored.
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