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
• Format: Article in Journal/Newspaper
• Language: English; Russian
• Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2019
• Subjects: precambrian; taimyr; neoproterozoic; collisional granite; geochronology; siberia paleocontinent; Science; Q; Kolosova; Pregradnaya; Taimyr; Siberia
• Online Access: https://doi.org/10.5800/GT-2019-10-4-0445; https://doaj.org/article/d7977839509a411ebbb3233733091b78

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...