New data on the geologic structure of the western part of the Zaisan folded area.
Abstract
The region under consideration is located in the western part of the Zaisan Hercynian folded region, bounded in the southwest by the Caledonian structures of the Chingiz-Tarbagatai middle mass (geoanticlinal zone of the first kind, according to V. A. Nikolaev) and in the northeast by the Charsky uplift (internal geoanticline of the second kind, according to V. A. Nikolaev) .....
Область исследования:
(Archived) Without section
Funding:
None
References
- Borukaev R. A. et al. Geology of the Chingiz geoanticlinoric zone (Central Kazakhstan). Tr. IGN AN KazSSR, vol. 5, 1962.
- Nekhoroshev V. P. Main phases of Hercynian tectogenesis, manifested in the Devonian and Lower Carboniferous in the Zaisan geosynclinal area. Mat-ly VSEGEI, nov. ser., iss. 19, 1956.
- Nekhoroshev V. P. Geology of Altai. Gosgeoltekhizdat, 1958.
- Sarycheva T. G., Sokolskaya A. N. On the Carboniferous and Permian complexes of brachiopods from some areas of South Siberia and Altai. Byull. MOIP, Otd. geol., iss. 6, 1959.
- Sevryugin N. A., Livshits M. B., Sindii I. K. Geological structure of the southwestern part of the Zaisan eugeosyncline. Mat-ly po geol. i polezn. iskop. Yuzhnogo Kazakhstana, iss. 3 (28). Alma-Ata, Nauka, 1965.
- Sokratov G. I. About the Upper Paleozoic of the Southern Kalba. Zapiski Gornogo Instituta, vol. XXXIII, iss. 2, 1958.
- Khisamutdinov M. G. Main features of tectonics and history of geological development of structural-formational zones of the Zaisan geosynclinal area. Mat-ly VSEGEI, nov. ser., t. 94, 1963.
- Khisamutdinov M. G. Formation complexes of the Zaisan geosynclinal area. Mat-ly VSEGEI, nov. ser., t. 111, 1964.
- Einor O. L. To the stratigraphy of the Upper Paleozoic of the Kalba Ridge. Izv. AN SSSR, ser. geol., No. 6, 1953.