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This study describes a new determination of the S and O isotope composition of Lower Permian (Kungurian) anhydrites from the Upper Pechora Basin, Cis-Ural region, Russia. δ34S values in sulphate facies vary from +13.7 to +15.1‰; and δ18O values range from +9.3 to +10.4‰. The values of d34S and d18O of anhydrite from halite facies varies from +12.6 to +15.0‰ and +7.5 to +10.9‰ respectively. The quantitative ratio of pyrite content from the water-insoluble residue (silty-sand fraction) is characterized by extremely low (<<1%) to high (4–5%) steep gradation values. The increased presence of pyrite indicates the influence of bacterial sulphate reduction. The sulphate reduction process was more intense, especially when evaporites were formed in mud. The narrow fluctuation range of sulphur and oxygen isotopes values of the measured anhydrite indicates low levels of fractionation. It was established that during the Permian, evolutionary changes in the content of sulphate ions in sea water correlate with the sulphur isotopic composition of marine evaporites
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
990--999
Opis fizyczny
Bibliogr. 51 poz., rys., tab., wykr.
Twórcy
autor
- National Academy of Sciences of Ukraine, Institute of Geology and Geochemistry of Combustible Minerals, Naukova, 3a, 79060 Lviv, Ukraine
autor
- Chinese Academy of Sciences, Nanjing Institute of Geology and Paleontology, State Key Laboratory of Paleobiology and Stratigraphy, Nanjing 210008, China
autor
- AGH University of Science and Technology, Faculty of Geology, Geophysics and Environment Protection, Al. A. Mickiewicza 30, 30-059 Kraków, Poland
autor
- Nanjing University, State Key Laboratory for Mineral Deposit Research, School of Earth Sciences and Engineering, Nanjing 210093, China
autor
- Institute of Geology of the Komi Science Center, Urals Branch of RAS, Pervomayskaya 54, 167610 Syktyvkar, Russia
autor
- “MIREKO” State Company, Gromova 75, 167983 Syktyvkar, Russia
Bibliografia
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- 32. Pankina, R.G., Mehdiyev, V.L., Guriev, S.M., 1985. Sulphur isotopic composition of modern and ancient evaporite formations halogen Caspian Depression (in Russian): 119-125. In: Lithofacial and Geochemical Problems of Salt Accumulation. Nauka, Moscow.
- 33. Peryt, T.M., Szaran, J., Jasionowski, M., Hałas, S., Peryt, D., Poberezhskyy, A., Karoli, S., Wojtowicz, A., 2002. S and O isotopic composition of the Middle Miocene Badenian sulphates in the Carpathian Foredeep. Geologica Carpathica, 53: 391-398.
- 34. Peryt, T.M., Tomassi-Morawiec, H., Czapowski, G., Hryniv, S.P., Pueyo, J.J., Eastoe, C.J., Vovnyuk, S., 2005. Polyhalite occurrence in the Werra (Zechstein, Upper Permian) Peribaltic Basin of Poland and Russia: evaporite facies constraints. Carbonates and Evaporites, 20: 182-194.
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- 42. Shekhunova, S.B., Stadnichenko, S.N., 2010. Features of sulphur isotopic composition of the Lower Permian saline formation of the Dnieper-Donets Basin (in Ukrainian). Zbirnik Naukove Pratse Institutu Geokhimii Navkolishnogo Seredovishcha, 18: 159-172.
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Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-aeb959d2-5b4f-497b-a9e8-dcc5f4d19756