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Rotation parameters of the Siberian domain and its eastern surrounding structures during different geological epochsстатья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 12 декабря 2016 г.
- Авторы: Timofeev V.Yu, Kazansky A.Yu, Ardyukov D.G., Metelkin D.V., Gornov P.Yu, Shestakov N.V., Timofeev A.V., Gil’manova G.Z.
- Журнал: Russian Journal of Pacific Geology
- Том: 5
- Номер: 4
- Год издания: 2011
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 288
- Последняя страница: 297
- DOI: 10.1134/S1819714011040075
- Аннотация: The motion of lithospheric blocks was analyzed in the junction zone between the Eurasian Plate and its surrounding structures. Its presentday stage was considered using GPS and seismologic data. Models of the movement of a rigid plate are considered for Eurasia. A model of Eurasia (northern part of Asia) was used to determine the rotation parameters of its southern periphery (Amur Plate) based on GPS data for the Far East (Sikhote Alin profile), and Transbaikal regions are shown as an example. A model of the Amur Plate was used to illustrate the behavior of the extension zone on its western boundary represented by the Lake Baikal depression during the Kultuk earthquake (M = 6.3, August, 27, 2008). Paleomagnetic data made it possible to determine the rotation pole of the Siberian Craton relative to its surrounding folded structures during the Mesozoic and to estimate its kinematic parameters. The permanent position of the rotation pole in the relative coordinate system since the terminal Paleozoic until the Recent indicates a constant rotation velocity of the Siberian domain within the Eurasian Plate structure.
- Добавил в систему: Казанский Алексей Юрьевич