Geomechanical conditions of the Tien Shan and Altai Orogeny

Тип публикации: статья из журнала

Год издания: 2017

Идентификатор DOI: 10.1134/S1028334X17100191

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. © 2017, Pleiades Publishing, Ltd.

Ссылки на полный текст

Издание

Журнал: Doklady Earth Sciences

Выпуск журнала: Vol. 476, Is. 2

Номера страниц: 1195-1199

ISSN журнала: 1028334X

Издатель: Maik Nauka-Interperiodica Publishing

Авторы

  • Suvorov V.D. (Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation)
  • Stefanov Y.P. (Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation, Institute of Strength Physics and Materials Science of Siberian Branch of Russian Academy of Sciences, Tomsk, Russian Federation)
  • Pavlov E.V. (Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation)
  • Melnik E.A. (Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation)
  • Tataurova A.A. (Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation, Novosibirsk national research state university, Novosibirsk, Russian Federation)
  • Kochnev V.A. (Federal Research Center Krasnoyarsk Scientific Center, Siberian Branch, Russian Academy of Sciences, Akademgorodok, Krasnoyarsk, Russian Federation)

Вхождение в базы данных

Информация о публикациях загружается с сайта службы поддержки публикационной активности СФУ. Сообщите, если заметили неточности.

Вы можете отметить интересные фрагменты текста, которые будут доступны по уникальной ссылке в адресной строке браузера.