THE MECHANISMS OF THE DISTRIBUTION OF HYDROTHERMAL-METASOMATIC GOLD- BEARING FORMATIONS (EAST OF THE SIBERIAN PLATFORM)

Authors

  • Z. Nikiforova FSBI Diamond and Precious Metal Geology Institute SB RAS

DOI:

https://doi.org/10.31618/nas.2413-5291.2021.1.74.517

Keywords:

metasomatites; deep faults; gold content; Siberian platform; placer gold; placers; deposit.

Abstract

Hydrothermal-metasomatic formations with Au content from 0.5 to 3.0 g/t, sometimes up to 24-32 g/t, were found in the east of the Siberian platform in the brecciated zones. They form, along ancient faults activated in the Mesozoic, extended narrow formations in terrigenous-carbonate and sandy layers of PZ-MZ age. The comparison of metasomatites with gold-ore metasomatites of the Kuranakh and Tabornoye deposits makes it possible for the first time to predict ore sources formed as a result of hydrothermal-metasomatic processes. Perhaps these sources represent a huge metallogenic potential.

Author Biography

Z. Nikiforova , FSBI Diamond and Precious Metal Geology Institute SB RAS

Doctor of Geological and Mineralogical Sciences, chief researcher

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Published

2021-12-30

Issue

Section

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