Ore-forming fluids of the gold-bearing interval of the Kola Superdeep Borehole

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Abstract

This paper reports on the physical-chemical parameters and vertical distribution of different types of fluid inclusions in quartz from the Au-bearing interval of the Kola Superdeep Borehole. We assume that gold ore mineralization was formed when a deep flux of CO2 interacted with brines at depths of 10 205-9269 m due to tectonic factors. In this paper, we discussed the role of these processes in the formation of the orogenic gold deposits including the gold mineralization of the Southern Pechenga structural zone.

About the authors

V. Yu. Prokofiev

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

Author for correspondence.
Email: vpr2004@rambler.ru
Russian Federation, 35, Staromonetny, Moscow, 119017

K. V. Lobanov

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

Email: vpr2004@rambler.ru

Corresponding Member of the Russian Academy of Sciences

Russian Federation, 35, Staromonetny, Moscow, 119017

A. A. Pek

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

Email: vpr2004@rambler.ru
Russian Federation, 35, Staromonetny, Moscow, 119017

M. V. Chicherov

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

Email: vpr2004@rambler.ru
Russian Federation, 35, Staromonetny, Moscow, 119017

A. A. Borovikov

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

Email: vpr2004@rambler.ru
Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090

References

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