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Nature of electric conductive layers of the upper crust and infrastructure of granites of the Central Tien Shan


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Abstract

We studied the infrastructure of granite massifs of the Central Tien Shan and its correlation with the electric conductive layer of the upper crust, which made possible to reveal new peculiarities of the structure of the granite layer in the region and to clarify the nature of low resistivity layers.

About the authors

A. K. Rybin

Scientific Station

Email: mgleonov@yandex.ru
Kyrgyzstan, Bishkek, 720049

M. G. Leonov

Geological Institute

Author for correspondence.
Email: mgleonov@yandex.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 109017

E. S. Przhiyalgovskii

Geological Institute

Email: mgleonov@yandex.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 109017

V. Yu. Batalev

Scientific Station

Email: mgleonov@yandex.ru
Kyrgyzstan, Bishkek, 720049

E. A. Bataleva

Scientific Station

Email: mgleonov@yandex.ru
Kyrgyzstan, Bishkek, 720049

V. D. Bragin

Scientific Station

Email: mgleonov@yandex.ru
Kyrgyzstan, Bishkek, 720049

Yu. A. Morozov

Schmidt Joint Institute of Physics of the Earth

Email: mgleonov@yandex.ru
Russian Federation, ul. Bolshaya Gruzinskaya 10, Moscow, 123810

G. G. Schelochkov

Scientific Station

Email: mgleonov@yandex.ru
Kyrgyzstan, Bishkek, 720049

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