East Mountain Crimea strain fields of different age

V. V. Gonchar


Actual data of kinematic analysis have been given, reconstruction and discrimination of strain fields with respect to the stage of main folding within the limits of the East Mountain Crimea have been fulfilled. The field of sub-meridional—northwestern compression realized in connection with processes of Arabian collision is responsible for formation of final folding of the Sudak-Karadag zone and post-folding collision compression of the East Mountain Crimea. As pre-folding fields arc defined the following ones: the fields of thrust-displacement type with northeastern and west-north-west orientations of compression axes and thrust fields with northeastern and northwestern orientation of axes of tension. The last ones can most probably be related to manifestation of riftogenesis behind the arc in the Black Sea region during Middle Cretaceous—Paleocene. The field of northeastern compression might be related to regional compression in Late Eocene—Oligocene, stipulated the folding of the Great Caucasus.


East Mountain Crimea; strain fields; folding; paleotectonic reconstructions


Byzova S. L., 1980. Some questions tectonics of the Crimean Mountains. Vestnik Moskovskogo universiteta. Ser. Ceologiya (6), 15—25 (in Russian).

Voznesenskiy A. I.,, Knipper A. L., Perfilyev A. S., Uspenskaya E. A., Areshin A. V., 1988. History of the eastern part of the Crimean Mountains terrane. Geotektonika (1), 27—44 (in Russian).

Geological map of the Crimean Mountains. 1:200 000. An explanatory note, 1984. Ed. N. E. Derenyuk. Kiev: Ministry of Geology of the USSR, 134 p. (in Russian).

Geology of the USSR. Vol. 8. Crimea. Part I. The geological description, 1969. Moscow: Nedra, 576 p. (in Russian).

Gonchar V. V., 2003. Stress field of the Crimean Mountains and geodynamic interpretation, Dopovidi NAN Ukrainy (3), 97—104 (in Russian).

Gonchar V. V., 2013. Sequence of stress fields and age of folding Eastern Mountain Crimea (according to the kinematic analysis taking into account the rotation of the layers). Geofizicheskiy zhurnal 35(4), 170—175 (in Russian).

Gonchar V. V., 2009. Postrift dive and age sub-oceanic depression. Geologiya і poleznye iskopaemye Mirovоgо okeana (2), 38—53 (in Russian).

Kazmin V. G., Lobkovskiy L. I., 2003. Geological structure and development of the Shatsky shaft. Proc.: Actual problems of oceanography. Moscow: Nauka, P. 221—243 (in Russian).

Kazmin V. G., Tikhonova N. E, 2006. Late Mesozoic-Eocene sea in the Black Sea-Caspian region: paleotectonic reconstruction. Geotektonika (3), 9—22 (in Russian).

Kizevalter D. S., Muratov M. V., 1959. Long-term development of geosynclinal folded structures of the eastern part of the Crimean Mountains. Izvestiya AN SSSR. Ser. geol. (5), 16—34 (in Russian).

Kopp M. L., Shcherba I. G., 1998. Caucasian basin in the Paleogene. Geotektonika (2), 29—50 (in Russian).

Marinin A. V., Saynto A., 2008. Comparison of the results researches palaeostresses Northwest Caucasus tectonophysical different methods. In: Problems tectonophysics. Moscow: Publ. House. IPE RAS, 225—243 (in Russian).

Mileev V. S., Baraboshkin E. Yu., Rozanov S. В., Rogov M. A., 2009. Tectonics and geodynamic evolution of the Crimean Mountains. Byulleten obshchestva ispytateley prirody. Otd. geol. 84 (is. 3), 3—23 (in Russian).

Murovskaya A. V., 2012. Stress-strain state of West Mountain Crimea in the Oligocene-Quaternary time of the tectonic data. Geofizicheskiy zhurnal 34(2), 109—119 (in Russian).

Murovskaya A., Sheremet E., Kolesnikova E., Lazarenko O., 2014, Deformations of the Upper Cretaceous—Neogene sediments of the South-western Crimea according to tectonophysical data. Geofizicheskiy zhurnal 36(6), 79—92 (in Russian).

Nikishin A. M., Korotaev M. V., Bolotov S. N., Ershov A. V., 2001. Tectonic history of the Black Sea basin. Byulleten obshchestva ispytateley prirody. Otd. geol. 76(is. 3), 3—18 (in Russian).

Nikishin A. M., Ershov A. V., Nikishin V. A., 2010. The geological history of the Western Caucasus and adjacent foredeeps based on analysis of the regional balanced section. Doklady AN 430(4), 515—517 (in Russian).

Panov D. I., 1997. On the question of the geological history of the Crimea in the Triassic and Jurassic time. Vestnik Moskovskogo universiteta. Ser. 4. Geologiya (3), 43—49 (in Russian).

Patalakha E. I., Gonchar V. V., Senchenkov I. K., Chervinko O. P., 2003, Indentorny mechanism in geodynamics Crimean Black Sea region. Forecast HC and seismic hazard. Kiev: ECMO, 226 p. (in Russian).

Patalakha E. I., Lukienko A. I., Gonchar V. V., 1995. Tectonic flows as a basis for understanding the geological structures. Kiev: Feniks, 160 p. (in Russian).

Tectonics of Ukraine, 1988. Eds S. S. Kruglov, A. K. Tsypko. Moscow: Nedra, 254 p. (in Russian).

Khain V. E., 1994. Tectonics Caucasus: current problems. Byulleten obshchestva ispytateley prirody. Otd. geol. 69(is. 5), 3—10 (in Russian).

Sheremet E., Sasson M., Gintov O., Müller C., Yegorova Т., Murovskaya A., 2014. Key problems of the eastern part of the Crimean Mountains stratigraphy. New micropaleontologic information for dating of flysch rocks. Geofizicheskiy zhumal 36(2), 35—56 (in Russian).

Shreyder Al. A., 2005. Disclosure of deep-water basin of the Black Sea. Okeanologiya (4), 592— 604 (in Russian).

Yudin V. V., Gerasimov M. E., 1997. Geodynamic model of the Crimean Black Sea and adjacent regions. In: Geodynamics of the Crimean-Black Sea region. Simferopol, P. 16—23 (in Russian).

Yudin V. V., Klochko A. A., 2001, Tectonics of the Eastern Crimea (Karadag). Raw material resources of the Crimea and offshore (oil and gas), Simferopol, 169—178 (in Russian).

Golmshtok A., Zonenshain L., Terekhov A., Shainurov R., 1992. Ago, thermal evolution and history of the Black Sea basin on heat flow and multichannel reflection data. Tectonophysics 210, 273—293.

Hyppolite J.C., 2002. Geodynamics of Dobrogea (Romania): new constraints on the evolution of the Tornquist—Teisseyre Line, the Black Sea and the Carpathians. Tectonophysics 357, 33— 53.

Navabrour P., Angelier J., Barrier E., 2007. Cenozoic post-colisional brittle tectonic history and stress reorientation in the High Zagros Belt (Iran, Pars Province). Tectonophysics 432, 101—131.

Saintot A., Angelier J., 2002. Tectonic paleostress fields and structural evolution of the NW-Caucasus fold-and-thrust belt from Late Cretaceous to Quaternary. Tectonophysics 357, 1—31.

Saintot A., Angelier J., Chorowicz J., 1999. Mechanical significance of structural patterns identified by remote sensing studies: a multiscale analysis of tectonic structures in Crimea. Tectonophysics 313, 187—218.

Sheremet Ye., Sosson M., Müller C., Gintov O., Murovskaya A., Yegorova Т., 2016. Key problems of stratigraphy in the Eastern Crimea Peninsula: some insights from new dating and structural data. In: Tectonic evolution of the Eastern Black Sea and Caucasus. Geol. Soc. Spec. Publ. London. Vol. 428. doi:10.1144/SP428.14

DOI: https://doi.org/10.24028/gzh.0203-3100.v39i1.2017.94011


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