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

Abstract 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 ty...

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Published in:Scientific Reports
Main Authors: Prokofiev, V. Yu., Banks, D. A., Lobanov, K. V., Selektor, S. L., Milichko, V. A., Akinfiev, N. N., Borovikov, A. A., Lüders, V., Chicherov, M. V.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2020
Subjects:
Online Access:http://dx.doi.org/10.1038/s41598-020-58020-8
http://www.nature.com/articles/s41598-020-58020-8.pdf
http://www.nature.com/articles/s41598-020-58020-8
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spelling crspringernat:10.1038/s41598-020-58020-8 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, V. Yu. Banks, D. A. Lobanov, K. V. Selektor, S. L. Milichko, V. A. Akinfiev, N. N. Borovikov, A. A. Lüders, V. Chicherov, M. V. 2020 http://dx.doi.org/10.1038/s41598-020-58020-8 http://www.nature.com/articles/s41598-020-58020-8.pdf http://www.nature.com/articles/s41598-020-58020-8 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Scientific Reports volume 10, issue 1 ISSN 2045-2322 Multidisciplinary journal-article 2020 crspringernat https://doi.org/10.1038/s41598-020-58020-8 2022-01-04T10:19:01Z Abstract 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 CO 2 , (2) liquid-vapor two-phase aqueous inclusions, (3) three-phase inclusions with NaCl daughter crystals, and (4) CO 2 -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 Springer Nature (via Crossref) Scientific Reports 10 1
institution Open Polar
collection Springer Nature (via Crossref)
op_collection_id crspringernat
language English
topic Multidisciplinary
spellingShingle Multidisciplinary
Prokofiev, V. Yu.
Banks, D. A.
Lobanov, K. V.
Selektor, S. L.
Milichko, V. A.
Akinfiev, N. N.
Borovikov, A. A.
Lüders, V.
Chicherov, M. V.
Exceptional Concentrations of Gold Nanoparticles in 1,7 Ga Fluid Inclusions From the Kola Superdeep Borehole, Northwest Russia
topic_facet Multidisciplinary
description Abstract 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 CO 2 , (2) liquid-vapor two-phase aqueous inclusions, (3) three-phase inclusions with NaCl daughter crystals, and (4) CO 2 -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, V. Yu.
Banks, D. A.
Lobanov, K. V.
Selektor, S. L.
Milichko, V. A.
Akinfiev, N. N.
Borovikov, A. A.
Lüders, V.
Chicherov, M. V.
author_facet Prokofiev, V. Yu.
Banks, D. A.
Lobanov, K. V.
Selektor, S. L.
Milichko, V. A.
Akinfiev, N. N.
Borovikov, A. A.
Lüders, V.
Chicherov, M. V.
author_sort Prokofiev, V. Yu.
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 Springer Science and Business Media LLC
publishDate 2020
url http://dx.doi.org/10.1038/s41598-020-58020-8
http://www.nature.com/articles/s41598-020-58020-8.pdf
http://www.nature.com/articles/s41598-020-58020-8
genre Northwest Russia
genre_facet Northwest Russia
op_source Scientific Reports
volume 10, issue 1
ISSN 2045-2322
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op_doi https://doi.org/10.1038/s41598-020-58020-8
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