EARLY NEOPROTEROZOIC GRANITOIDS IN THE RYAZANOVSKY MASSIF OF THE YENISEI RIDGE AS INDICATORS OF THE GRENVILLE OROGENY AT THE WESTERN MARGIN OF THE SIBERIAN CRATON | Nozhkin | Geodynamics & Tectonophysics

Geodynamics & Tectonophysics
Geodinamika i tektonofizika

ISSN 2078-502X (Online)

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Nozhkin A.D., Turkina O.M., Likhanov I.I., Ronkin Yu.L. EARLY NEOPROTEROZOIC GRANITOIDS IN THE RYAZANOVSKY MASSIF OF THE YENISEI RIDGE AS INDICATORS OF THE GRENVILLE OROGENY AT THE WESTERN MARGIN OF THE SIBERIAN CRATON. Geodynamics & Tectonophysics. 2024;15(2):0745. (In Russ.) https://doi.org/10.5800/GT-2024-15-2-0745. EDN: ORDEGX

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ISSN 2078-502X (Online)

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Sklyarov E.V.

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About the Authors

A. D. Nozhkin
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090

O. M. Turkina
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090

I. I. Likhanov
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090

Yu. L. Ronkin
Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences
Russian Federation

15 Academician Vonsovsky St, Ekaterinburg 620016

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