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

Авторлар: 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
Мекемелер:
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
Шығарылым: Том 476, № 2 (2017)
Беттер: 1195-1199
Бөлім: Geophysics
URL: https://ogarev-online.ru/1028-334X/article/view/191127
DOI: https://doi.org/10.1134/S1028334X17100191
ID: 191127

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Аннотация

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.

Авторлар туралы

V. Suvorov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch

Хат алмасуға жауапты Автор.
Email: SuvorovVD@ipgg.sbras.ru
Ресей, 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
Ресей, Novosibirsk, 630090; Tomsk, 634005