Origin of the Badenian salts from East Slovakian basin indicated by the analysis of fluid inclusions

• Autorzy: Galamay A. R. , Bukowski K. , Poberezhskyy A. V. , Karoli S. , Kovalevych V. M.
• Języki publikacji: EN

Abstrakty

EN

Chemical composition of the brines of primary fluid inclusions in sedimentary halite (from the boreholes: P-2, P-3, P-6, P-7 and P-8) of the Badenian evaporite of the Zbudza Fm. from East Slovakian basin indicates that the basinal brines belong to the Na-K-Mg-Cl-SO₄ type. The ratios of K+, Mg²⁺, and SO₄^2- ions are practically the same as they were in the Badenian seawater. Taking into account the information on the chemical evolution of seawater in the Phanerozoic (Kovalevich et al., 1998) and the calculations of this evolution for the Cenozoic (Zimmermann, 2000) it is suggested that the Badenian seawater was characterized by the reduced contents of Mg (by approximately 20%) and SO₄^2- (by approximately 40%) in comparison with the recent seawater. The postsedimentary recrystallization of salts occurred under the effect of buried brines, which inherited their composition from the primary basinal brines. The intensive recrystallization of salts occurred during the tectonic movements.

Słowa kluczowe

EN

Miocene; evaporites; halite; fluid inclusions; Carpathian region

• Wydawca: Polskie Towarzystwo Geologiczne
• Czasopismo: Annales Societatis Geologorum Poloniae
• Rocznik: 2004
• Tom: Vol. 74, No 3
• Strony: 267--276
• Opis fizyczny: Bibliogr. 51 poz., tab., wykr.

Twórcy

autor

Galamay A. R.

• Institute of Geology and Geochemistry of Combustible Minerals, National Academy of Sciences of Ukraine, Naukova 3A, 79053 Lviv, Ukraine

autor

Bukowski K.

• Faculty of Geolog}’, Geophysics and Environment Protection, University of Science and Technology, Mickiewicza 30, 30-059 Kraków, Poland

autor

Poberezhskyy A. V.

• Institute of Geology and Geochemistry of Combustible Minerals, National Academy of Sciences of Ukraine, Naukova 3A, 79053 Lviv, Ukraine

autor

Karoli S.

• Geological Survey of Slovak Republic, Werferova 1, 04011 Košice 1, Slovakia

autor

Kovalevych V. M.

• Institute of Geology and Geochemistry of Combustible Minerals, National Academy of Sciences of Ukraine, Naukova 3A, 79053 Lviv, Ukraine

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