Phanerozoic evolution model of a stressstrain state of the Earth crust at the Dnieper-Donets paleorift

Author:

Bartashchuk O.V.,

Publisher

National Academy of Sciences of Ukraine (Co. LTD Ukrinformnauka)

Reference15 articles.

1. 1. Chebanenko, I. I. (1977). Theoretical aspects of tectonic divisibility of the earth's crust. Kiev: Nauk. Dumka (in Russian).

2. 2. Gintov, O. B. (2005). Field tectonophysics and its application in the study of deformations of the earth's crust of Ukraine. Kiev: Feniks (in Russian).

3. Structures of horizontal shift of sedimentary basins and experience of application of tectonophysical methods to increase prospecting and exploration efficiency and mastering nearshift oil;Timurziev;Heofiz,2014

4. 4. Markov, G. A. & Savchenko, S. N. (1984). Stress state of rocks and rock pressure in mountainous terrain structures. Leningrad: Nauka (in Russian).

5. 4. Goryaynov, S. V. (1999). About Alpine complication of geological structure in various regions of Ukraine. Dopov. Nac. acad. nauk Ukr., No. 8, pp. 106-111 (in Russian).

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