Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia)
- Authors: Gibsher N.A.1, Sazonov A.M.2, Travin A.V.1,3,4, Tomilenko A.A.1, Ponomarchuk A.V.1, Sil’yanov S.A.2, Nekrasova N.A.2, Shaparenko E.O.1, Ryabukha M.A.1, Khomenko M.O.1
-
Affiliations:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
- Institute of Mining, Geology, and Geotechnology, Siberian Federal University
- Novosibirsk State University
- Novosibirsk State Technical University
- Issue: Vol 57, No 5 (2019)
- Pages: 593-599
- Section: Short Communications
- URL: https://journals.rcsi.science/0016-7029/article/view/156186
- DOI: https://doi.org/10.1134/S0016702919050033
- ID: 156186
Cite item
Abstract
40Ar/39Ar dates on the quartz–micaceous–sulfide, quartz–gold–arsenopyrite–pyrrhotite, and quartz–gold–stibium associations at the superlarge (>1000 t Au) Olimpiada gold deposit, the Yenisei Ridge, are compared. It is established that the hydrothermal activity at the deposit has continued for no less than 150 Ma from 817 to 660 Ma.
Keywords
About the authors
N. A. Gibsher
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
A. M. Sazonov
Institute of Mining, Geology, and Geotechnology, Siberian Federal University
Author for correspondence.
Email: sazonov_am@mail.ru
Russian Federation, pr. Svobodnyi 79, Krasnoyarsk, 660041
A. V. Travin
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University; Novosibirsk State Technical University
Author for correspondence.
Email: travin@igm.nsc.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090; ul. Pirogova 1, Novosibirsk, 630090; pr. K. Marksa 20, Novosibirsk, 630073
A. A. Tomilenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
A. V. Ponomarchuk
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
S. A. Sil’yanov
Institute of Mining, Geology, and Geotechnology, Siberian Federal University
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Svobodnyi 79, Krasnoyarsk, 660041
N. A. Nekrasova
Institute of Mining, Geology, and Geotechnology, Siberian Federal University
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Svobodnyi 79, Krasnoyarsk, 660041
E. O. Shaparenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
M. A. Ryabukha
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Author for correspondence.
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
M. O. Khomenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: marya.ryabukha@mail.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
Supplementary files
