U–Pb Isotope and REE Composition of Zircon from the Pyroxene Crystalline Schists of the Irkut Terrane, Sharyzhalgai Uplift: Evidence for the Neoarchean Magmatic and Metamorphic Events
| dc.contributor.author | Turkina O.M. | |
| dc.contributor.author | Berezhnaya N.G. | |
| dc.contributor.author | Urmantseva L.N. | |
| dc.contributor.author | Paderin I.P. | |
| dc.contributor.author | Skublov S.G. | |
| dc.date.accessioned | 2024-04-18T00:08:57Z | |
| dc.date.available | 2024-04-18T00:08:57Z | |
| dc.date.issued | 2009 | |
| dc.description.abstract | The Early Precambrian granulite-gneissic complexes are typically characterized by a long evolutionary history, which involves formation of their protoliths and repeated metamorphism related mainly with collisional events. Zircons from high-grade metamorphic rocks usually consist of cores inherited from the protolith, and one or several mantles and rims that were formed during later metamorphism or partial melting. High-resolution methods of U–Pb dating make it possible to determine the age of cores and rims. | ru_RU |
| dc.identifier.citation | Doklady Earth Sciences, 2009, Vol. 429A, No. 9, pp. 1505–1510 | ru_RU |
| dc.identifier.doi | 10.1134/S1028334X09090207 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/43608 | |
| dc.language.iso | en | ru_RU |
| dc.subject | Zircon | ru_RU |
| dc.subject | Irkut Terrane | ru_RU |
| dc.subject | Sharyzhalgai Uplift | ru_RU |
| dc.subject | Neoarchean | ru_RU |
| dc.subject.age | Докембрий::Архей::Неоархейская | |
| dc.subject.age | Precambrian::Archean::Neoarchean | |
| dc.title | U–Pb Isotope and REE Composition of Zircon from the Pyroxene Crystalline Schists of the Irkut Terrane, Sharyzhalgai Uplift: Evidence for the Neoarchean Magmatic and Metamorphic Events | ru_RU |
| dc.type | Article | ru_RU |