Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia

In the drill core of the Kola super-deep borehole (SG-3, 12,262 m depth) gold-bearing rocks of Archaean age have been located at depths of 9,500 to 11,000 m. In veins, between 9,052 and 10,744 m, within this gold zone, quartz contains fluid inclusions with gold nanoparticles. There are 4 types of fl...

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Main Authors: Prokofiev, VY, Banks, DA, Lobanov, KV, Selektor, SL, Milichko, VA, Akinfiev, NN, Borovikov, AA, Lüders, V, Chicherov, MV
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2020
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Online Access:https://eprints.whiterose.ac.uk/155466/
https://eprints.whiterose.ac.uk/155466/3/s41598-020-58020-8.pdf
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spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:155466 2023-05-15T17:46:05+02:00 Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia Prokofiev, VY Banks, DA Lobanov, KV Selektor, SL Milichko, VA Akinfiev, NN Borovikov, AA Lüders, V Chicherov, MV 2020-01-24 text https://eprints.whiterose.ac.uk/155466/ https://eprints.whiterose.ac.uk/155466/3/s41598-020-58020-8.pdf en eng Nature Publishing Group https://eprints.whiterose.ac.uk/155466/3/s41598-020-58020-8.pdf Prokofiev, VY, Banks, DA orcid.org/0000-0001-9118-5298 , Lobanov, KV et al. (6 more authors) (2020) Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia. Scientific Reports, 10. 1108. ISSN 2045-2322 cc_by_4 CC-BY Article NonPeerReviewed 2020 ftleedsuniv 2023-01-30T22:25:47Z In the drill core of the Kola super-deep borehole (SG-3, 12,262 m depth) gold-bearing rocks of Archaean age have been located at depths of 9,500 to 11,000 m. In veins, between 9,052 and 10,744 m, within this gold zone, quartz contains fluid inclusions with gold nanoparticles. There are 4 types of fluid inclusions (1) gas inclusions of dense CO2, (2) liquid-vapor two-phase aqueous inclusions, (3) three-phase inclusions with NaCl daughter crystals, and (4) CO2-aqueous inclusions. In all inclusion types, there are extremely high concentrations of gold. The highest gold concentrations were found in the type 3 and 4 fluid inclusions with an average concentration of c. 750 ppm and may be as high as 6,000 ppm. The presence of gold as nanoparticles in the solutions of these fluid inclusions was determined by optical and spectroscopic methods. We suggest that these fluids could be a precursor of “orogenic gold fluids” which, at the gold concentrations determined, would reduce the requirements for large volumes of metamorphic fluids to form orogenic ore deposits. Further, as nanoparticles, gold could be transported in larger amounts than in true solution. Article in Journal/Newspaper Northwest Russia White Rose Research Online (Universities of Leeds, Sheffield & York)
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
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language English
description In the drill core of the Kola super-deep borehole (SG-3, 12,262 m depth) gold-bearing rocks of Archaean age have been located at depths of 9,500 to 11,000 m. In veins, between 9,052 and 10,744 m, within this gold zone, quartz contains fluid inclusions with gold nanoparticles. There are 4 types of fluid inclusions (1) gas inclusions of dense CO2, (2) liquid-vapor two-phase aqueous inclusions, (3) three-phase inclusions with NaCl daughter crystals, and (4) CO2-aqueous inclusions. In all inclusion types, there are extremely high concentrations of gold. The highest gold concentrations were found in the type 3 and 4 fluid inclusions with an average concentration of c. 750 ppm and may be as high as 6,000 ppm. The presence of gold as nanoparticles in the solutions of these fluid inclusions was determined by optical and spectroscopic methods. We suggest that these fluids could be a precursor of “orogenic gold fluids” which, at the gold concentrations determined, would reduce the requirements for large volumes of metamorphic fluids to form orogenic ore deposits. Further, as nanoparticles, gold could be transported in larger amounts than in true solution.
format Article in Journal/Newspaper
author Prokofiev, VY
Banks, DA
Lobanov, KV
Selektor, SL
Milichko, VA
Akinfiev, NN
Borovikov, AA
Lüders, V
Chicherov, MV
spellingShingle Prokofiev, VY
Banks, DA
Lobanov, KV
Selektor, SL
Milichko, VA
Akinfiev, NN
Borovikov, AA
Lüders, V
Chicherov, MV
Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
author_facet Prokofiev, VY
Banks, DA
Lobanov, KV
Selektor, SL
Milichko, VA
Akinfiev, NN
Borovikov, AA
Lüders, V
Chicherov, MV
author_sort Prokofiev, VY
title Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
title_short Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
title_full Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
title_fullStr Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
title_full_unstemmed Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
title_sort exceptional concentrations of gold nanoparticles in 1,7 ga fluid inclusions from the kola superdeep borehole, northwest russia
publisher Nature Publishing Group
publishDate 2020
url https://eprints.whiterose.ac.uk/155466/
https://eprints.whiterose.ac.uk/155466/3/s41598-020-58020-8.pdf
genre Northwest Russia
genre_facet Northwest Russia
op_relation https://eprints.whiterose.ac.uk/155466/3/s41598-020-58020-8.pdf
Prokofiev, VY, Banks, DA orcid.org/0000-0001-9118-5298 , Lobanov, KV et al. (6 more authors) (2020) Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia. Scientific Reports, 10. 1108. ISSN 2045-2322
op_rights cc_by_4
op_rightsnorm CC-BY
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