ABSTRACT: Hydrogeological structures in Šarišský Štiavnik and Radoma can be classified as combined hydrogeological structures, where the upper partial hydrogeological structure is opened (Magura unit) and the lower structure is semi-closed (unit Obidowa - Slopnice - Zboj). Mineral waters are formed on the tectonic fault zones of the Zlín formation and Makovica sandstones. Precipitation waters flow downwards thus getting enriched in T.D.S. content. The process is enhanced by inflow of CO2 rich mineral waters of the Obidowa - Slopnice - Zboj unit, pushed by carbon dioxide and methane. Gaseous mineral waters uplift to the ground surface on the barrier of the Malcov formation in the form of barrier-fissure springs.
bibliografický odkaz na článok:
Marcin, D., 2002: Hydrogeologické štruktúry Šarišský Štiavnik a Radoma.- Podzemná voda ISSN 1335-1052, VIII, 2/2002, 116-122.
jazyk článku:
kľúčové slová:
Západné Karpaty, flyšové pásmo východného Slovenska, minerálne vody, hydrogeologická štruktúra
key words:
Western Carpathians, Flysch belt of the Eastern Slovakia, mineral waters, hydrogeological structure
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