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The northward continental drift component in the Phanerozoic, its possible cause, and structural consequencesстатья
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: 21 июля 2014 г.
- Авторы: Goncharov M.A., Raznitsyn Yu N., Barkin Yu V.
- Журнал: Doklady Earth Sciences
- Том: 455
- Номер: 2
- Год издания: 2014
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 383
- Последняя страница: 385
- DOI: 10.1134/S1028334X14050031
- Аннотация: The northern component of continental drift in the Phanerozoic, at the beginning of which the continents were concentrated in the southern hemisphere, resulted in their accumulation in the northern hemisphere, and the accompanying submeridional compression of both the continental and oceanic lithosphere produced north vergent thrusting. In contrast to this situation, currently the South Pole area is occupied by the highly raised continent of Antarctica while the North Pole is encircled with the Arctic Ocean, which has an abnormally wide shelf with a thick sedimentary cover rich in hydrocarbons. Continental drift was accompanied and most likely was caused by axisymmetric convection in the mantle with an upward flow at the South Pole and a downward flow in the North Pole area. A likely cause of all these phenomena is the northward drift of the Earth’s core.
- Добавил в систему: Гончаров Михаил Адрианович
Прикрепленные файлы
| № | Имя | Описание | Имя файла | Размер | Добавлен |
|---|---|---|---|---|---|
| 1. | Полный текст | 2014_DAN_CONTINENTS_S_N.pdf | 163,1 КБ | 3 декабря 2014 [BarkinYV] |