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.
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ACKNOWLEDGMENTS
We are grateful to reviewers for constructive comments taken into account in the final version of the manuscript.
This work was supported by the Russian Science Foundation (project no. 14-17-00602P) and Russian Foundation for Basic Research (project no. 17-05-00936). Mineralogical and thermochronological studies were carried out in the framework of the state task of the Institute of Geology and Mineralogy of the Siberian Branch of the Russian Academy of Sciences (project nos. 0330-2016-0005 and 0330-2016-0013).
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Gibsher, N.A., Sazonov, A.M., Travin, A.V. et al. Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia). Geochem. Int. 57, 593–599 (2019). https://doi.org/10.1134/S0016702919050033
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DOI: https://doi.org/10.1134/S0016702919050033