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Chemical composition of Badenian brines from primary fluid inclusions in halite (Transcarpathian Basin, Ukraine)
Języki publikacji
Abstrakty
W strukturach wzrostowych halitu typu szewron w basenie zakarpackim (Ukraina) stwierdzono występowanie pierwotnych inkluzji, które mogą być pomocne przy określeniu składu chemicznego solanek badeńskiego basenu ewaporatowego. Ciekłe inkluzje występujące w sedymentacyjnym halicie badane były metodą analizy ultramikrochemicznej. Koncentracja solanek zakarpackiego basenu była wysoka - zbliżona do średniego etapu sedymentacji halitu. Zawartość jonów: K+ zawierała się w przedziale 10.6-17.6 g/l, Mg2+ w zakresie 31.4-58.3 g/l, a SO4 2- w przedziale 22.4-39.0 g/l. Na podstawie badań składu chemicznego głównych jonów stwierdzono, że solanki basenu zakarpackiego były nasycone względem halitu i podobne do solanek z innych badeńskich basenów.
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, Mg2+ from 31.4 g/l to 58.3 g/l, and SO4 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.
Wydawca
Rocznik
Tom
Strony
245--267
Opis fizyczny
Bibliogr. [43], rys., tab., wykr.
Twórcy
autor
- Instytut Geologii i Geochemii Narodowej Akademii Nauk Ukrainy; ul. Naukowa 3a, 79-060 Lwów, Ukraina
autor
- AGH Akademia Górniczo-Hutnicza, Wydział Geologii, Geofizyki i Ochrony OErodowiska; al. A. Mickiewicza 30, 30-059 Kraków
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-AGHL-0003-0004