The Geology, Mineral Associations, and Composition of Native Gold in the Mineral Deposits of the Taimyr–Severnaya Zemlya Orogen


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Аннотация

The variety of sizes and morphology of grains and chemical composition of native Au, and the diversity of mineral productive associations in the new ore occurrences of the Western and Central Taimyr (the Minina–Bolshevik miogeocline and the Shrenk–Faddeevskaya accretionary mineragenic zones) indicate the complex multicomponent composition of ore-forming systems and different physicochemical conditions of the formation of gold ore mineralization. The native Au characteristics and specific features of the geological structure of the objects point to the significant gold ore potential of the Central Sector of the Russian Arctic.

Авторлар туралы

V. Proskurnin

Karpinsky Russian Geological Research Institute

Email: palyan@igm.nsc.ru
Ресей, St. Petersburg, 199106

G. Palyanova

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

Хат алмасуға жауапты Автор.
Email: palyan@igm.nsc.ru
Ресей, Novosibirsk, 630090; Novosibirsk, 630090

A. Gavrish

Karpinsky Russian Geological Research Institute

Email: palyan@igm.nsc.ru
Ресей, St. Petersburg, 199106

B. Petrushkov

Karpinsky Russian Geological Research Institute

Email: palyan@igm.nsc.ru
Ресей, St. Petersburg, 199106

A. Bagaeva

Karpinsky Russian Geological Research Institute

Email: palyan@igm.nsc.ru
Ресей, St. Petersburg, 199106

N. Bortnikov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

Email: palyan@igm.nsc.ru
Ресей, Moscow, 119017

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© Pleiades Publishing, Ltd., 2019