The Ages and Isotope Compositions of the Gold–Silver Deposits and Occurrences of the Evensk Group (Okhotsk–Chukotka Volcanogenic Belt, Northeast Russia)

Author:

Kravtsova R. G.,Dril S. I.,Makshakov A. S.

Publisher

Pleiades Publishing Ltd

Reference68 articles.

1. O. V. Avchenko, A. S. Vakh, N. A. Goryachev, I. A. Aleksandrov, T. A. Velivetskaya, and I. N. Kapitonov, “Genesis of the Berezitovoe gold–polymetallic deposit: evidence from the isotope composition of lead, oxygen, and sulfur,” Dokl. Earth Sci. 453 (1), 1117–1120 (2013).

2. V. V. Akinin, A. N. Glukhov, G. O. Polzunenkov, A. V. Alshevsky, and D. I. Alekseev, “The age of the Kubaka epithermal gold-silver deposit (Omolon Massif, Northeast Russia): geological and isotopic-geochronological constrains (U-Pb and 40Ar/39Ar methods),” Russ. J. Pac. Geol. 14 (1), 32–42 (2020).

3. Examples of consistent and inconsistent age values determined by different methods and relative to the geological position of the studied object;G. D. Afanas’ev,1973

4. E. V. Beloglazov, “Peculiarities of geological structure and lithochemical aureoles of the Irbychan ore field,” Proc. Geology and Mineral Resources of Northeast USSR (Magadan, 1982), pp. 132–137 [in Russian].

5. V. F. Belyi, Stratigraphy and Structures of the Okhotsk–Chukotka Volcanogenic Belt (Nauka, Moscow, 1977) [in Russian].

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