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The neotectonics and geodynamic development of the Naryk-Ostashkin Area (South Kuznetsk Basin)

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Abstract

A complex of studies, including structural-geomorphological analysis, statistical processing of satellite-image data, and satellite radar interferometry allowed us to identify the arch-block pattern of modern dislocations in the study area, to reveal the nature of their relationship with ancient complexes, and to estimate the velocity of modern vertical movements. According to the geodynamic model that was developed using the IramRMS software, the formation of the modern structure occurred under the conditions of north-western horizontal compression (330°).

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Authors and Affiliations

  1. Department of Geology, Moscow State University, Moscow, 119991, Russia

    L. V. Panina & V. A. Zaitsev

  2. Schmidt Institute of physics of the Earth, Russian Academy of Sciences, Bol’shaya Gruzinskaya ul. 10, Moscow, 123995, Russia

    V. O. Mikhailov

Authors
  1. L. V. Panina
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  2. V. A. Zaitsev
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  3. V. O. Mikhailov
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Corresponding author

Correspondence to L. V. Panina.

Additional information

Original Russian Text © L.V. Panina, V.A. Zaitsev, V.O. Mikhailov, 2015, published in Vestnik Moskovskogo Universiteta. Geologiya, 2015, No. 1, pp. 20–26.

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Panina, L.V., Zaitsev, V.A. & Mikhailov, V.O. The neotectonics and geodynamic development of the Naryk-Ostashkin Area (South Kuznetsk Basin). Moscow Univ. Geol. Bull. 70, 18–23 (2015). https://doi.org/10.3103/S0145875215010056

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  • DOI: https://doi.org/10.3103/S0145875215010056

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