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Northern Peri-Tethyan Cenozoic intraplate deformations: influence of the Tethyan collision belt on the Eurasian continent from Paris to Tian-Shanстатья
Информация о цитировании статьи получена из
Scopus,
Web of Science
Дата последнего поиска статьи во внешних источниках: 18 декабря 2013 г.
- Авторы: Nikishin A.M., Brunet M.F., Cloetingh S., Ershov A.V.
- Журнал: COMPTES RENDUS DE L ACADEMIE DES SCIENCES DE L URSS
- Том: 324
- Номер: 1
- Год издания: 1997
- Первая страница: 49
- Последняя страница: 57
- Аннотация: During the Oligocene-Holocene Tethyan collisional tectonics, compressional deformations of two recognizable types developed inside the Northern Peri-Tethyan areas up to 1500 km to the North of the collision front: long-wave (400-600 km) deformations of topography (vertical amplitude 200-500 m), and inversional thrusting/folding. The Black Sea and Southern Caspian basins experienced rapid subsidence at the same time. The compressional structures and the long wavelength intraplate deformations of topography would result from gentle whole-lithospheric folds. The dynamics of the intraplate compression is complex: stress related to collision, ridge push, plate-driving forces, and Oligocene-Neogene global plate kinematic reorganizations.
- Добавил в систему: Никишин Анатолий Михайлович