Geomechanical conditions of the Tien Shan and Altai Orogeny


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Abstract

The results of numerical modelling of deformation of the Earth’s crust along the Tarim–Altai profile caused by the force of gravity and lateral compression using the approximate two-dimensional model of the elastoplastic transition are presented. The conditions of the formation of mountains and their roots were determined taking into account some geological and geophysical parameters.

About the authors

V. D. Suvorov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Author for correspondence.
Email: SuvorovVD@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090

Yu. P. Stefanov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch; Institute of Strength Physics and Materials Science of Siberian Branch of Russian Academy of Sciences

Email: SuvorovVD@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090; Tomsk, 634005

E. V. Pavlov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Email: SuvorovVD@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090

E. A. Melnik

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Email: SuvorovVD@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090

A. A. Tataurova

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch; Novosibirsk national research state university

Email: SuvorovVD@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk

V. A. Kochnev

Federal Research Center Krasnoyarsk Scientific Center, Siberian Branch

Email: SuvorovVD@ipgg.sbras.ru
Russian Federation, Akademgorodok, Krasnoyarsk, 660036

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