Geochemical features of Paleozoic Au–Ag epithermal deposits (Northeastern Russia)


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The geochemical features and conditions of formation of the Paleozoic epithermal Au–Ag mineralization in the pre-accretion Kedon (D2–3) volcanoplutonic belt located within the Omolon craton terrain are described. The new data on the composition and contents of trace and rare-earth elements (REEs) in igneous ores of epithermal deposits is provided. The elevated grades of a wide range of trace elements as compared to the average values of the upper crust have been identified.

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A. Volkov

Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

编辑信件的主要联系方式.
Email: tma2105@mail.ru
俄罗斯联邦, Moscow, 119017

A. Sidorov

Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tma2105@mail.ru
俄罗斯联邦, Moscow, 119017

N. Savva

Shilo Northeastern Complex Scientific Research Institute, Far East Branch

Email: tma2105@mail.ru
俄罗斯联邦, Magadan, 685010

E. Kolova

Shilo Northeastern Complex Scientific Research Institute, Far East Branch

Email: tma2105@mail.ru
俄罗斯联邦, Magadan, 685010

K. Murashov

Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tma2105@mail.ru
俄罗斯联邦, Moscow, 119017

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