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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… Click to show full abstract
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.
Keywords:
geochemical features;
features paleozoic;
northeastern russia;
paleozoic epithermal;
epithermal deposits;
deposits northeastern
Journal Title: Doklady Earth Sciences
Year Published: 2017
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Journal Title: Doklady Earth Sciences
Year Published: 2017
Link to full text (if available)
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recommendations!