Geomechanical conditions of the Tien Shan and Altai Orogeny


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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.

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V. Suvorov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

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Email: SuvorovVD@ipgg.sbras.ru
俄罗斯联邦, Novosibirsk, 630090

Yu. 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
俄罗斯联邦, Novosibirsk, 630090; Tomsk, 634005

E. Pavlov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Email: SuvorovVD@ipgg.sbras.ru
俄罗斯联邦, Novosibirsk, 630090

E. Melnik

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Email: SuvorovVD@ipgg.sbras.ru
俄罗斯联邦, Novosibirsk, 630090

A. Tataurova

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

Email: SuvorovVD@ipgg.sbras.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

V. Kochnev

Federal Research Center Krasnoyarsk Scientific Center, Siberian Branch

Email: SuvorovVD@ipgg.sbras.ru
俄罗斯联邦, Akademgorodok, Krasnoyarsk, 660036

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