Geologicheskii Vestnik

The upper, relatively thin shell of our planet, called the Earth’s crust, is composed of geological matter of several levels of organization, for each of which a special structure is peculiar. Therefore, geological matter and structure are the main subjects of study in any theory of the formation of the earth’s crust. No exception are nappes (sharriages). But if the latter is such a structure, then sufficient attention is paid to all the problems associated with the geological substance that were not even considered previously. However, without matter there can be neither the earth’s crust nor the theory of its formation. The problems associated with the matter of the earth’s crust were solved in a number of individual works of TT. Kazantseva. The problems of the origin and development of the geological substance of the active zones of the folded areas are provided and developed. In a different way, the issues of formational analysis, the frequency of geological events are resolved. A new understanding of tectonic stages, cycles and stages has been introduced. The evolution of sediment accumulation and magmatism is considered from a different position than was previously accepted.

structure, sharriages, thrusts, allochthons, formations, magmatism, metamorphism, ore formation, oil and gas accumulation, patterns of development, evolution, geodynamics

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• Kamaletdinov M.A., Kazantsev Yu.V., Kazantseva T.T. Proiskhozhdenie skladchatosti [Origin of folding]. M.: Nauka, 1981. 135 p. (In Russian).
• Kamaletdinov M.A., Kazantseva T.T., Kazantsev Yu.V. Osnovnyye voprosy formirovaniya zemnoy kory Urala v paleozoye [The main questions of the formation of the crust of the Urals in the Paleozoic]. Ufa: BFAN SSSR, 1978. 31 p.
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• Kazantsev Yu.V., Kazantseva T.T., Kamaletdinov M.A., Arzhavitina M.Yu., Arzhavitin P.V., Khairullina F.V. Strukturnaya geologiya Magnitogorskogo sinklinoriya Yuzhnogo Urala [Structural Geology of the Magnitogorsk Synclinorium of the Southern Urals]. M.: Nauka, 1992. 183 p. (In Russian).
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• Kazantseva T.T. Tektonicheskie tsikly i formatsionnye ryady [Tectonic cycles and formation series]. Ufa, 1983. 37 p. (In Russian).
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• Kazantseva T.T. Allokhtonnye struktury i formirovanie zemnoi kory Urala [Allochthonousstructures and the formation of the crust of the Urals]. M.: Nauka, 1987. 169 p. (In Russian). Kazantseva T.T. Tektonika i evoliutsiya [Tectonics and evolution]. Ufa: IG BNTS UrO AN SSSR, 1990. 40 p. (In Russian).
• Kazantseva T.T. Osnovy shariazhno-nadvigovoi teorii formirovaniya zemnoi kory [Fundamentals of the thrust theory of the formation of the earth's crust] // Geologiya.Izv. Otd. nauk o Zemle i prirodnykh resursov AN RB. 2000. No 5. P. 15–46 (In Russian).
• Kazantseva T.T. Geodinamicheskaya model' rudogeneza [Geodynamic model of ore genesis] // Georesources. 2012. No. 8 (50). P. 3–9 (In Russian).
• Kazantseva T.T. Fundamentalnye teorii evoliutsii zemnoi kory [Basic theories on the evolution of the Earth’s crust] // Vestnik ANRB. 2015. V.20, No.3(79). P. 14–27 (In Russian).
• Kazantseva T.T., Kamaletdinov M.A. The Geosynclinal development of the Urals // Tectonophysics. 1986. V. 127, No. 3–4. P. 371–381. doi.org/10.1016/0040-1951(86)90071-5.
• Kazantseva T.T., Kazantsev Yu.V. Strukturnyi faktor v teoreticheskoi geologii[Structural factorin theoretical geology]. Ufa: Gilem, 2010. 327 p. (In Russian).
• Kazantseva T.T., Kamaletdinov M.A., Kazantsev Yu.V., Zufarova N.A. Proiskhozhdenie nefti [Origin of oil]. Ufa, 1982. 30 p. (In Russian).
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• Smirnov G.A. Razvitie nauchnykh vzglyadov na dinamiku Ural'skoi gornoi sistemy [Development of scientific views on the dynamics of the Ural mountain system]. Ekaterinburg: Nauka. Ural'skoe otd., 1992. 295 p. (In Russian).