| Автор | Sengör, A. M. Celâl |
| Автор | Natal'in, Boris A. |
| Дата выпуска | 1996 |
| dc.description | ▪ Abstract Turkic-type orogeny is a class of collisional mountain building, in which the precollision history of one, or both, of the colliding continents involves the growth of very large, subcontinent-size subduction-accretion complexes, into which magmatic arc axes commonly migrate and thus enlarge the continent to which they are attached. A review of the evolution of two Phanerozoic (Altaids, Nipponides), one Neoproterozoic (East African), and one Archean (Yilgarn) Turkic-type orogens shows that this type of orogeny may have been the principal builder of the continental crust through recorded Earth history. The total juvenile material added to Turkic-type orogens at any one time in the Phanerozoic seems close to 1 km<sup>3</sup>/year, which about equals the amount of material annually fed into the mantle at subduction zones. As some 0.02 to 0.03% of that material is generally agreed to return to the crust by arc magmatism, these figures provide a minimum net growth rate for the continental crust during the Phanerozoic. |
| Формат | application.pdf |
| Издатель | Annual Reviews |
| Копирайт | Annual Reviews |
| Название | TURKIC-TYPE OROGENY AND ITS ROLE IN THE MAKING OF THE CONTINENTAL CRUST |
| DOI | 10.1146/annurev.earth.24.1.263 |
| Print ISSN | 0084-6597 |
| Журнал | Annual Review of Earth and Planetary Sciences |
| Том | 24 |
| Первая страница | 263 |
| Последняя страница | 337 |
| Аффилиация | Sengör, A. M. Celâl; İstanbul Teknik Üniversitesi, Maden Fakltesi, Jeoloji Bölümü, Ayazağa İstanbul, 80626 Turkey |
