40Ar/39Ar Age of the Burinda Gold–Silver Deposit and Its Relationship to Magmatism (Northeastern Part of the Argun Superterrane)


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Abstract

Our investigations have made it possible to estimate the age of hydrothermal ore metasomatic rocks at the Burinda Au–Ag deposit, one of the best known in East Asia, at 126–128 Ma. This deposit was formed due to hydrothermal processes at the final development stages of the Taldan volcanic complex.

About the authors

I. V. Buchko

Institute of Geology and Nature Management, Far East Branch, Russian Academy of Sciences

Email: travin@uiggm.nsc.ru
Russian Federation, Blagoveshchensk, 675000

A. A. Sorokin

Institute of Geology and Nature Management, Far East Branch, Russian Academy of Sciences

Email: travin@uiggm.nsc.ru
Russian Federation, Blagoveshchensk, 675000

V. A. Ponomarchuk

Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Author for correspondence.
Email: ponomar@igm.nsk.ru
Russian Federation, Novosibirsk, 630090

A. V. Travin

Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences; Tomsk State University

Author for correspondence.
Email: travin@uiggm.nsc.ru
Russian Federation, Novosibirsk, 630090; Tomsk, Tomsk oblast, 634050

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