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Get Free AccessOxidation zone of the Yubileinoe massive sulfide deposit, South Urals, is buried beneath Jurassic sediments containing coalified plant remains. Mineralogy of gossan of this deposit is marked by the abundance of siderite. The carbon isotope composition (δ13C) in siderite varies from -20.0 to -23.4‰ PDB, which is close to δ13C variation in coals from the overlying sediments (-23.5 to -26.2‰ PDB). The formation of siderite is likely related to interaction between solutions of the Triassic oxidation zone and fermentation products of the organic matter.
Konstantin ‘kostya’ Novoselov, Е. В. Белогуб, С. А. Садыков, I. V. Vikentyev (2019). Gossan of the Yubileynoe massive sulfide deposit (South Urals): evidence for formation on the seafloor. Литология и полезные ископаемые, 1(1), pp. 90-100, DOI: 10.31857/s0024-497x2019190-100.
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Type
Article
Year
2019
Authors
4
Datasets
0
Total Files
0
Language
English
Journal
Литология и полезные ископаемые
DOI
10.31857/s0024-497x2019190-100
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