HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS
The article considers textural and structural features of hematite-carbonate rocks associated with carbonate-sulfide clastic ores of the Yubileynoe massive sulfide deposit, South Urals. Some hematitecarbonate rocks exhibit signatures of the replacement of sulfide clasts and hyaloclasts by hematite-c...
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South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
2024-12-01
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Series: | Минералогия |
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Online Access: | https://journal.mineralogy.ru/wp-content/uploads/2025/01/2024_10_4_3.pdf |
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author | A.S. Tseluyko N.R. Ayupova D.A. Artemyev M.A. Rassomakhin V.A. Kotlyarov |
author_facet | A.S. Tseluyko N.R. Ayupova D.A. Artemyev M.A. Rassomakhin V.A. Kotlyarov |
author_sort | A.S. Tseluyko |
collection | DOAJ |
description | The article considers textural and structural features of hematite-carbonate rocks associated with carbonate-sulfide clastic ores of the Yubileynoe massive sulfide deposit, South Urals. Some hematitecarbonate rocks exhibit signatures of the replacement of sulfide clasts and hyaloclasts by hematite-carbonate material, classified as carbonate analogs of gossanites. The hematite-carbonate aggregates after sulfide clasts are characterized by inherited reniform-colloform, radial and crystalline-granular structures, as well as the inclusions of relict sulfides and tellurides. The hematite-carbonate aggregates after sulfide clasts contain the elevated concentrations of chalcophile (Cu, Zn, Pb, As, Sb, Bi, Te) and lithophile (Ti, Zr, V, W) trace elements. The hematite-carbonate clasts after hyaloclasts contain aggregates with globular structure and syneresis cracks and contain relics of chlorite. The matrix of hematite-carbonate rocks consists of calcite with inclusions and aggregates of dolomite, chlorite, quartz and apatite. Late sulfide mineralization (pyrite metacrystals, aggregates and veins of chalcopyrite and sphalerite) is characteristic of both hematite-carbonate rocks after sulfide clasts and hyaloclasts. |
format | Article |
id | doaj-art-418fdf8d513242fdb87873587f1de40e |
institution | Kabale University |
issn | 2313-545X 2782-2044 |
language | English |
publishDate | 2024-12-01 |
publisher | South Urals Federal Research Center of Mineralogy and Geoecology UB RAS |
record_format | Article |
series | Минералогия |
spelling | doaj-art-418fdf8d513242fdb87873587f1de40e2025-02-06T10:30:12ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442024-12-01104607410.35597/2313-545X-2024-10-4-3HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTSA.S. Tseluyko0N.R. Ayupova1D.A. Artemyev2M.A. Rassomakhin3V.A. Kotlyarov4South Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASThe article considers textural and structural features of hematite-carbonate rocks associated with carbonate-sulfide clastic ores of the Yubileynoe massive sulfide deposit, South Urals. Some hematitecarbonate rocks exhibit signatures of the replacement of sulfide clasts and hyaloclasts by hematite-carbonate material, classified as carbonate analogs of gossanites. The hematite-carbonate aggregates after sulfide clasts are characterized by inherited reniform-colloform, radial and crystalline-granular structures, as well as the inclusions of relict sulfides and tellurides. The hematite-carbonate aggregates after sulfide clasts contain the elevated concentrations of chalcophile (Cu, Zn, Pb, As, Sb, Bi, Te) and lithophile (Ti, Zr, V, W) trace elements. The hematite-carbonate clasts after hyaloclasts contain aggregates with globular structure and syneresis cracks and contain relics of chlorite. The matrix of hematite-carbonate rocks consists of calcite with inclusions and aggregates of dolomite, chlorite, quartz and apatite. Late sulfide mineralization (pyrite metacrystals, aggregates and veins of chalcopyrite and sphalerite) is characteristic of both hematite-carbonate rocks after sulfide clasts and hyaloclasts.https://journal.mineralogy.ru/wp-content/uploads/2025/01/2024_10_4_3.pdfhematite-carbonate gossanitessubmarine hypergenesishalmyrolyisishyaloclastssulfidestelluridesla-icp-msyubileynoe massive sulfide deposit |
spellingShingle | A.S. Tseluyko N.R. Ayupova D.A. Artemyev M.A. Rassomakhin V.A. Kotlyarov HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS Минералогия hematite-carbonate gossanites submarine hypergenesis halmyrolyisis hyaloclasts sulfides tellurides la-icp-ms yubileynoe massive sulfide deposit |
title | HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS |
title_full | HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS |
title_fullStr | HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS |
title_full_unstemmed | HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS |
title_short | HEMATITE-CARBONATE ROCKS OF THE YUBILEYNOE MASSIVE SULFIDE DEPOSIT (SOUTH URALS): EVIDENCE OF REPLACEMENT OF SULFIDE CLASTS AND HYALOCLASTS |
title_sort | hematite carbonate rocks of the yubileynoe massive sulfide deposit south urals evidence of replacement of sulfide clasts and hyaloclasts |
topic | hematite-carbonate gossanites submarine hypergenesis halmyrolyisis hyaloclasts sulfides tellurides la-icp-ms yubileynoe massive sulfide deposit |
url | https://journal.mineralogy.ru/wp-content/uploads/2025/01/2024_10_4_3.pdf |
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