The pre‐Vendian (640–610 ma) granite magmatism in the Central Taimyr fold belt: the final stage of the Neoproterozoic evolution of the Siberian paleocontinent active margin

• Published in: Geodynamics & Tectonophysics
• Main Authors: A. B. Kuzmichev, M. K. Danukalova, V. F. Proskurnin, A. A. Bagaeva, N. I. Beresyuk, P. A. Gromov, А. Б. Кузьмичев, М. К. Данукалова, В. Ф. Проскурнин, А. А. Багаева, Н. И. Березюк, П. А. Громов
• Other Authors: We are grateful to A.N. Larionov for the isotopic dating of zircons. Our studies were supported by the Russian Foundation for Basic Research (Grants 16-05- 00176 and 19-05-00926). The study of A.B. Kuzmichev and M.K. Danukalova was part of the GIN RAS Research Programme (No. 0135-2019-0051).
• Format: Article in Journal/Newspaper
• Language: English
• Published: Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch 2019
• Subjects: Сибирский палеоконтинент; Taimyr; Neoproterozoic; collisional granite; geochronology; Siberia Paleocontinent; Таймыр; неопротерозой; коллизионные граниты; геохронология; Kolosova; Pregradnaya; Arctic; Polarforschung; Siberia
• Online Access: https://www.gt-crust.ru/jour/article/view/934; https://doi.org/10.5800/GT-2019-10-4-0445

Eastern part of the Central Taimyr belt is composed of Precambrian rocks penetrated by granites of the Snezhnaya complex (845–825 million years) and later overlain by mid‐Neoproterozoic sin‐ postorogenic sedimentary deposits of the Stanovaya‐Kolosova Group. Two competing concepts on the Precambrian...