RELATION BETWEEN δ 13 С, δ 18 О AND REE CONTENT IN CARBONATITES OF THE TOMTOR COMPLEX, SAKHA REPUBLIC (YAKUTIA) | Ponomarchuk | Geodynamics & Tectonophysics

Geodynamics & Tectonophysics
Geodinamika i tektonofizika

ISSN 2078-502X (Online)

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Ponomarchuk V.A., Lazareva E.V., Zhmodik S.M., Travin A.V., Tolstov A.V. RELATION BETWEEN δ¹³С, δ¹⁸О AND REE CONTENT IN CARBONATITES OF THE TOMTOR COMPLEX, SAKHA REPUBLIC (YAKUTIA). Geodynamics & Tectonophysics. 2024;15(5):0785. (In Russ.) https://doi.org/10.5800/GT-2024-15-5-0785. EDN: UHDVTF

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ISSN 2078-502X (Online)

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About the Authors

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

3 Academician Koptyug Ave, Novosibirsk 630090

E. V. Lazareva
Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

3 Academician Koptyug Ave, Novosibirsk 630090

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

3 Academician Koptyug Ave, Novosibirsk 630090

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

3 Academician Koptyug Ave, Novosibirsk 630090

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

3 Academician Koptyug Ave, Novosibirsk 630090

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