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

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

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...

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Bibliographic Details
Main Authors: A. B. Kuzmichev, M. K. Danukalova, V. F. Proskurnin, A. A. Bagaeva, N. I. Beresyuk, P. A. Gromov
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2019-12-01
Series:Геодинамика и тектонофизика
Subjects:
precambrian
taimyr
neoproterozoic
collisional granite
geochronology
siberia paleocontinent
Online Access:https://www.gt-crust.ru/jour/article/view/934

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