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Fluid Inclusion Evidences for the P-T Conditions of Quartz Veins Formation in the Black Shale-Hosted Gold Deposits, Bodaybo Ore Region, Russia

  • Natalia N. AnkushevaEmail author
  • Ekaterina E. Palenova
  • Svetlana N. Shanina
Article
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Abstract

The P-T conditions of auriferous and barren quartz veins from Kopylovsky, Kavkaz and Krasnoye gold deposits in Proterozoic black shales of Bodaybo ore region are presented the first time in this study. Fluid inclusions trapped in auriferous quartz are aqueous Na±K-Mg chloride with salinity of 6 wt.%–8.8 wt.% NaCleqv. Homogenization temperatures vary from 260 to 350 °С, and calculated trapping pressures are 1.2–1.6 kbar. The fluids trapped in barren quartz have more complicated compositions with Na, K, Mg and Fe chlorides, salinity up to 13 wt.% NaCleqv, and homogenization temperatures ranging between 140 and 280 °С. The volatiles in fluids are dominated by H2O, followed by CO2 with minor amounts of CH4 and N2. We suppose that auriferous and barren quartz veins have been formed due to the basic metamorphogenic fluid as evidenced by the close slat and gas fluid composition.

Key Words

Bodaybo black shales gold deposits gold-bearing quartz barren veins fluid inclusions P-T conditions 

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Notes

Acknowledgments

This study was partially supported by the State Contract of the Institute of Mineralogy, South-Urals Federal Research Center of Mineralogy and Geoecology, Urals Branch, Russian Academy of Sciences (Project for 2019–2021) and the Basic Research Foundation of Russia (No. 16-05-00580). Sincere thanks go to the reviewers and the editors for their suggestions. The final publication is available at Springer via  https://doi.org/10.1007/s12583-019-1024-5.

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Copyright information

© China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature 2019

Authors and Affiliations

  1. 1.Institute of Mineralogy, South-Urals Federal Research Center of Mineralogy and GeoecologyUrals Branch, Russian Academy of SciencesMiassRussia
  2. 2.Geological DepartmentSouth-Urals State UniversityMiassRussia
  3. 3.Institute of Geology of the Komi Science Center, Urals BranchRussian Academy of SciencesSyktyvkarRussia

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