Аннотация
The results of geochronological (U–Pb, Ar–Ar), geochemical, and isotopic (Sr, Nd) studies of the Ordovician and Devonian mafic volcanic–subvolcanic rock associations of the Minusinsk Depression are presented. The obtained ages of magmatic associations and the basite composition, considering previous studies, witness to the impact of two mantle plumes different in age (Late Cambrian–Ordovician and Devonian) on suprasubduction rock complexes in active continental margin settings.
Язык оригинала | английский |
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Страницы (с-по) | 184-189 |
Число страниц | 6 |
Журнал | Doklady Earth Sciences |
Том | 472 |
Номер выпуска | 2 |
DOI | |
Состояние | Опубликовано - 1 фев 2017 |