For citations:
Kuzmichev A.B., Danukalova M.K., Proskurnin V.F., Bagaeva A.A., Beresyuk N.I., Gromov P.A. 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. Geodynamics & Tectonophysics. 2019;10(4):841-861. https://doi.org/10.5800/GT-2019-10-4-0445
Email this article 