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Moscow University Geology Bulletin

, Volume 73, Issue 3, pp 238–246 | Cite as

A Kinematic Model of the Formation of the Sim Trough of the Uralian Foredeep

  • Al. V. Tevelev
  • I. A. Prudnikov
  • Ark. V. Tevelev
  • A. O. Khotylev
  • E. A. Volodina
Article
  • 6 Downloads

Abstract

The structural features and mechanism of the formation of the Sim trough within the Uralian Foredeep, as well as the development of the entire Karatau–Suleiman block, are considered. This wedge-shaped block was subject to lateral extrusion to the north along conjugated strike-slip fault zones under a general latitudinal compression. This factor determined the local meridional compression and latitudinal extension of the block. In the central part of the block, the latitudinal extension was compensated by gradual subsidence, which resulted in the formation of the Sim trough.

Keywords

Urals foreland basin structural assemblages fold strike-slip fault transpression 

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Copyright information

© Allerton Press, Inc. 2018

Authors and Affiliations

  • Al. V. Tevelev
    • 1
  • I. A. Prudnikov
    • 1
  • Ark. V. Tevelev
    • 1
  • A. O. Khotylev
    • 1
  • E. A. Volodina
    • 1
  1. 1.Department of GeologyMoscow State UniversityMoscowRussia

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