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Specific Features in the Deep Structure of the Naryn Basin–Baibichetoo Ridge–Atbashi Basin System: Evidence from the Complex of Geological and Geophysical Data

Authors
  • Rybin, A. K.1
  • Bataleva, E. A.1
  • Morozov, Yu. A.2
  • Leonov, M. G.3
  • Batalev, V. Yu.1
  • Matyukov, V. E.1
  • Zabinyakova, O. B.1
  • Nelin, V. O.1
  • 1 Russian Academy of Sciences, Scientific Station, Bishkek, Kyrgyzstan , Bishkek (Kyrgyzstan)
  • 2 Russian Academy of Sciences, Schmidt Institute of Physics of the Earth, Moscow, 123810, Russia , Moscow (Russia)
  • 3 Russian Academy of Sciences, Geological Institute, Moscow, 119017, Russia , Moscow (Russia)
Type
Published Article
Journal
Doklady Earth Sciences
Publisher
Pleiades Publishing
Publication Date
Apr 01, 2018
Volume
479
Issue
2
Pages
499–502
Identifiers
DOI: 10.1134/S1028334X18040165
Source
Springer Nature
License
Yellow

Abstract

New magnetotelluric data were obtained for the Karabuk profile crossing the Naryn basin–Baibichetoo Ridge–Atbashi basin geodynamic system (Central Tien-Shan). The complex geological–geophysical cross section along the profile provides a good agreement between the surface tectonic structures and the deep geoelectric model. The electric conductivity anomalies revealed as subvertical conductors striking along the flanks of basins may be explained by the zones of dynamic influence of faults and cataclasis of granite.

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