Geomechanical conditions of the Tien Shan and Altai Orogeny

V. D. Suvorov; Yu. P. Stefanov; E. V. Pavlov; E. A. Melnik; A. A. Tataurova; V. A. Kochnev

doi:10.1134/S1028334X17100191

Geomechanical conditions of the Tien Shan and Altai Orogeny

Autores: Suvorov V.D.¹, Stefanov Y.P.¹^,2, Pavlov E.V.¹, Melnik E.A.¹, Tataurova A.A.¹^,3, Kochnev V.A.⁴
Afiliações:
1. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch
2. Institute of Strength Physics and Materials Science of Siberian Branch of Russian Academy of Sciences
3. Novosibirsk national research state university
4. Federal Research Center Krasnoyarsk Scientific Center, Siberian Branch
Edição: Volume 476, Nº 2 (2017)
Páginas: 1195-1199
Seção: Geophysics
URL: https://journals.rcsi.science/1028-334X/article/view/191127
DOI: https://doi.org/10.1134/S1028334X17100191
ID: 191127

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Resumo

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.

Sobre autores

V. Suvorov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Autor responsável pela correspondência
Email: SuvorovVD@ipgg.sbras.ru
Rússia, 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
Rússia, Novosibirsk, 630090; Tomsk, 634005