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Access status: Open Access ,
Skład izotopów tlenu i siarki w badeńskich siarczanach występujących w złożu solnym Zbudza (Słowacja)
(Wydawnictwa AGH, 2009) Kasprzyk, Alicja; Bukowski, Krzysztof
In the Zbudza salt deposit (East Slovakian Basin) sulphates occur in the form of singly nodules or layers of nodular anhydrite, in the form of laminated anhydrite and gypsum, anhydritic breccia and type of matrix in the siliciclastics. Oxygen and sulphur isotope contents of the anhydrite were determined in 10 point samples taken from wells P-6 and P-7 located in the middle part of East Slovakian Basin. With the exception of two samples the oxygen and sulphur isotope compositions of analyzed anhydrite samples show a narrow spectrum scatter of $\delta$-values ($\delta ^{18}O$: 12.34-13.15‰, $\delta ^{34}S$: 22.08-24.45‰). Overall, these results correspond well to the isotopic composition of Badenian anhydrites in the Carpathian Foredeep and associated with halite in Wieliczka and Bochnia salt deposits. Similar $\delta ^{18}O$ and $\delta ^{34}S$ were also documented for the Badenian primary gypsum deposits in the Carpathian Foredeep in Poland, Czech Republic and Ukraine.
Access status: Open Access ,
Skład chemiczny badeńskich solanek z pierwotnych ciekłych inkluzji w halicie, basen zakarpacki (Ukraina)
(Wydawnictwa AGH, 2011) Galamay, Anatolyi R.; Bukowski, Krzysztof
The primary fluid inclusions, which may be helpful in detemining the chemical composition of brines in the Badenian evaporite basin, were found in the chevron halite crystals from the Transcarpathian Basin (Ukraine). Fluid inclusions in sedimentary halite were examined with the use of ultra-microchemical analysis. Concentration of brines was high - close to the middle stage of halite sedimentation. The content of ions: K$^{+}$ ranged from 10.6 g/l to 17.6 g/l, Mg$^{2+}$ from 31.4 g/l to 58.3 g/l, and SO$_{4}^{2-}$ from 22.4 g/l to 39.0 g/l. Based on the chemical composition of major ions it was concluded that the brine from the Transcarpathian basin was saturated (to the stage of halite crystallization) and was similar to the Badenian brines from other basins.
Access status: Open Access ,
Salt geology and mining traditions: Kalush and Stebnyk mines (Fore-Carpathian region, Ukraine)
(Wydawnictwa AGH, 2009) Bukowski, Krzysztof; Czapowski, Grzegorz
Development of industrial underground salt mining in western Ukraine has started in the mid-19th century with the discovery of large potash-magnesium salt deposits in Kalush (1854) and Stebnyk (1901). Potash salts concentrations occur within the Miocene sedimentary complexes of Ukrainian Carpathian Foredeep (correlated with the successions observed in the Polish part of Carpathian Foredeep) as isolated lenses or compressed folded layers of varied extent. Thickness of exploited potash seams varies from 4 m up to 150 m and the main mineral is sylvine, accompanied also by carnallite, kainite and langbeinite. Both Kalush and Stebnyk mines, now closed, belong to the first places in the world, where exploitation of potash salts were realized. Their unique historical character, documenting the salt exploitation traditions in this region and evolution of mining techniques, ought to be widely advertised as the valid points of Ukrainian-Polish cross-border geotouristic route, named »Traces of large extinct mammals, earth wax, oil and salt«.
Access status: Open Access ,
Salt resources in Poland at the beginning of the 21st century
(Wydawnictwa AGH, 2012) Czapowski, Grzegorz; Bukowski, Krzysztof
W pracy przedstawiono aktualny stan wiedzy o udokumentowanych (bilansowych i pozabilansowych) zasobach soli kamiennej i soli potasowej w Polsce oraz scharakteryzowano ich oszacowane zasoby przewidywane do głębokości 2 km. Dominującą rolę w bilansie zasobowym odgrywają sole kamienne wieku późnopermskiego (ok. 95% zasobów udokumentowanych i blisko 99.9% zasobów przewidywanych), udział soli wieku mioceńskiego jest podrzędny. Większość (blisko 69%) zasobów udokumentowanych kryje się w wysadach solnych, zaś zasobów przewidywanych - w złożach pokładowych (96.7%). Udokumentowane zasoby soli kamiennej wystarczą na 26 000 lat (przy aktualnej wielkości wydobycia), zaś zasoby przewidywane na ponad 500 lat (przy wykorzystaniu 1/10[6] części zasobów). Zasoby bilansowe późnopermskich soli potasowo-magnezowych w nieeksploatowanych udokumentowanych pięciu złożach wynoszą ponad 669 mln t, z czego większość (cztery złoża, powyżej 597 mln t) stanowią złoża typu polihalitowego. Zasoby przewidywane tych soli oszacowano na blisko 1.02 mld t.
Access status: Open Access ,
Mioceńskie sole kamienne i potasowe zachodniej Ukrainy: Seminarium geologiczno-górnicze Polskiego Stowarzyszenia Górnictwa Solnego pt. Złoża soli na kresach wschodnich dawnej Rzeczpospolitej
(Wydawnictwa AGH, 2009) Czapowski, Grzegorz; Poborska-Młynarska, Katarzyna; Bukowski, Krzysztof
In the end of May 2008 the Polish Salt Mining Society had organized the field seminar focused on development and exploitation of rock and potash salt deposits of the Miocene age, occurred in the Western Ukraine. Actually the exploitation of all salt deposits in the Western Ukraine was stopped in last several years because of complicated geological-hydrological conditions, intensive salt karst phenomena and extensive former salt excavation. It caused that although the former agreements the visiting of underground mine chambers and surface salt quarries (in Kałusz and Sołotwino structures the salts pierced up to the surface) was too danger and in the both visited deposits their geology and methods of salt exploitation were only reported by miners in the office.

Bukowski, Krzysztof

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