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


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详细

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.

作者简介

E. Bataleva

Scientific Station

编辑信件的主要联系方式.
Email: bataleva@gdirc.ru
吉尔吉斯斯坦, Bishkek

E. Przhiyalgovskii

Geological Institute

Email: bataleva@gdirc.ru
俄罗斯联邦, Moscow, 119017

V. Batalev

Scientific Station

Email: bataleva@gdirc.ru
吉尔吉斯斯坦, Bishkek

E. Lavrushina

Geological Institute

Email: bataleva@gdirc.ru
俄罗斯联邦, Moscow, 119017

M. Leonov

Geological Institute

Email: bataleva@gdirc.ru
俄罗斯联邦, Moscow, 119017

V. Matyukov

Scientific Station

Email: bataleva@gdirc.ru
吉尔吉斯斯坦, Bishkek

A. Rybin

Scientific Station

Email: bataleva@gdirc.ru
吉尔吉斯斯坦, Bishkek

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