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    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 by A. B. Kuzmichev, M. K. Danukalova, V. F. Proskurnin, A. A. Bagaeva, N. I. Beresyuk, P. A. Gromov

    Published 2019-12-01
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