Geochemical features of Paleozoic Au–Ag epithermal deposits (Northeastern Russia)
- Авторлар: Volkov A.V.1, Sidorov A.A.1, Savva N.E.2, Kolova E.E.2, Murashov K.Y.1
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Мекемелер:
- Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Shilo Northeastern Complex Scientific Research Institute, Far East Branch
- Шығарылым: Том 472, № 2 (2017)
- Беттер: 178-183
- Бөлім: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/189288
- DOI: https://doi.org/10.1134/S1028334X17020088
- ID: 189288
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
A. Volkov
Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Хат алмасуға жауапты Автор.
Email: tma2105@mail.ru
Ресей, Moscow, 119017
A. Sidorov
Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tma2105@mail.ru
Ресей, Moscow, 119017
N. Savva
Shilo Northeastern Complex Scientific Research Institute, Far East Branch
Email: tma2105@mail.ru
Ресей, Magadan, 685010
E. Kolova
Shilo Northeastern Complex Scientific Research Institute, Far East Branch
Email: tma2105@mail.ru
Ресей, Magadan, 685010
K. Murashov
Institute for Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tma2105@mail.ru
Ресей, Moscow, 119017
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