New data on the deep structure of the South Kochkor zone of concentrated deformation


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

Based on a complex study of the upper crust structure in the southern margin of Kochkor basin (Northern Tien Shan), including study of the structure of the Cenozoic sedimentary cover, the deep geoelectrical structure, the structural unconformities, and occurrences of recent deformations in the basement rocks, new geological–geophysical cross sections are constructed. The cross sections show both fault structures that penetrate the cover from the basement and flat interplate detachments with related fold-overthrust structures. The comparison of the cross sections has established the absence of common planes of fault extensions along the entire margin of the hollow, except for the zone where the margin and the hollow adjoin, which can be caused by the zones of dynamic influence of secondary faults, the zones of fracturing, and the zones of cataclasis of blockwise disintegrated granite massifs.

About the authors

E. A. Bataleva

Scientific Station

Author for correspondence.
Email: bataleva@gdirc.ru
Kyrgyzstan, Bishkek

E. S. Przhiyalgovskii

Geological Institute

Email: bataleva@gdirc.ru
Russian Federation, Moscow, 119017

V. Yu. Batalev

Scientific Station

Email: bataleva@gdirc.ru
Kyrgyzstan, Bishkek

E. V. Lavrushina

Geological Institute

Email: bataleva@gdirc.ru
Russian Federation, Moscow, 119017

M. G. Leonov

Geological Institute

Email: bataleva@gdirc.ru
Russian Federation, Moscow, 119017

V. E. Matyukov

Scientific Station

Email: bataleva@gdirc.ru
Kyrgyzstan, Bishkek

A. K. Rybin

Scientific Station

Email: bataleva@gdirc.ru
Kyrgyzstan, Bishkek

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2017 Pleiades Publishing, Ltd.